Singer/songwriter Miles played a acoustic set supporting Average Sex.

Image by Clyde Foster

 

Two image sets from last night. Seeing was average/below average.

There is some nice activity taking place.

Regarding the Hellas disturbance:

a) It appears to me that this is a “mixed cloud”, including a reasonable level of dust.

b) The cloud seems to have changed shape and consolidated/concentrated a bit, although take note of my comment f), below.

c) The “subtle” linear cloud extending WNW of Hellas that I noted yesterday is very clearly seen in the 18.10UT image.

d) It is my view that the 18.10UT image links the linear cloud with the Hellas disturbance, hence I would be tempted to refer to it as a “plume”. Ie It appear that material is being blown out of Hellas and driven in a WNW direction. Other views/comments would be welcome.

e) It appears that the plume is quite dynamic. Note in the 18.50UT image(only 40mins later), that the rim of Hellas is visible where the plume crosses it, which is not the case in the earlier image.

f) When rapidly switching between todays 18.50UT image(I deliberately tried to capture the same CM) and the 18.11 image from yesterday, a lot of changes in and around Hellas are noted. It appears that there is a lot of dissipation of material across Hellas and also in the close surroundings. The indication is that the disturbance has had quite a wide influence.

Over and above the Hellas disturbance, there is a large cloud front adjacent(following) to the NPC which has developed over the last 24hrs. The following edge of the front is notably sharp. There is also quite a concentrated cloud formation on the preceding side of the NPC.

Beautiful afternoon reflections on the Loch.

 

Loch Linnhe is a sea loch on the west coast of Scotland. The part upstream of Corran is known in Gaelic as An Linne Dhubh (the black pool, originally known as Loch Abar), and downstream as An Linne Sheileach (the salty pool). The name Linnhe is derived from the Gaelic word linne, meaning "pool".

 

Loch Linnhe follows the line of the Great Glen Fault, and is the only sea loch along the fault. About 50 kilometres (31 mi) long, it opens onto the Firth of Lorne at its southwestern end. The part of the loch upstream of Corran is 15 kilometres (9.3 mi) long and an average of about 2 kilometres (1.2 mi) wide. The southern part of the loch is wider, and its branch southeast of the island of Lismore is known as the Lynn of Lorne. Loch Eil feeds into Loch Linnhe at the latter's northernmost point, while from the east Loch Leven feeds in the loch just downstream of Corran and Loch Creran feeds into the Lynn of Lorne. The town of Fort William lies at the northeast end of the loch, at the mouth of the River Lochy.

Average Joe with a moustache on a late 19th Century arcade tintype.

Taken in average and OK - but not great - 'seeing' conditions in the early hours of 28 October 2012, after a month in the UK where hardly any astrophotography has been possible thanks to the cloudy and wet weather. The Great Red Spot and surrounding area seems to have changed fairly dramatically since last year although it will need excellent seeing conditions to see better detail around it.

 

This was also a first test for me of using an Atmospheric Dispersion Corrector to see if I could improve the blue channel in particular.

 

Peter

 

Equipment used:

DMK21AU mono CCD, ADC, 1.25" RGB filters, 2.5x Powermate, 12" Meade LX200 SCT.

Average seeing. 25th May 2019 21:44 UTC,

 

Transparency (3/5)

Seeing (2.5/5)

 

C9.25 Edge HD

ZWO 120MC-S

Winjupos

AutoStakkert

An average of 250,000 passengers use the Bernina Express annually. Already during the provision and cleaning of the train there is a crowd. Switzerland, June 1, 2023. (2/3)

The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1,283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them.

 

The various geyser basins are located where rainwater and snowmelt can percolate into the ground, get indirectly superheated by the underlying Yellowstone hotspot, and then erupt at the surface as geysers, hot springs, and fumaroles. Thus flat-bottomed valleys between ancient lava flows and glacial moraines are where most of the large geothermal areas are located. Smaller geothermal areas can be found where fault lines reach the surface, in places along the circular fracture zone around the caldera, and at the base of slopes that collect excess groundwater. Due to the Yellowstone Plateau's high elevation the average boiling temperature at Yellowstone's geyser basins is 199 °F (93 °C). When properly confined and close to the surface it can periodically release some of the built-up pressure in eruptions of hot water and steam that can reach up to 390 feet (120 m) into the air (see Steamboat Geyser, the world's tallest geyser). Water erupting from Yellowstone's geysers is superheated above that boiling point to an average of 204 °F (95.5 °C) as it leaves the vent. The water cools significantly while airborne and is no longer scalding hot by the time it strikes the ground, nearby boardwalks, or even spectators. Because of the high temperatures of the water in the features it is important that spectators remain on the boardwalks and designated trails. Several deaths have occurred in the park as a result of falls into hot springs.

 

Prehistoric Native American artifacts have been found at Mammoth Hot Springs and other geothermal areas in Yellowstone. Some accounts state that the early people used hot water from the geothermal features for bathing and cooking. In the 19th century Father Pierre-Jean De Smet reported that natives he interviewed thought that geyser eruptions were "the result of combat between the infernal spirits". The Lewis and Clark Expedition traveled north of the Yellowstone area in 1806. Local natives that they came upon seldom dared to enter what we now know is the caldera because of frequent loud noises that sounded like thunder and the belief that the spirits that possessed the area did not like human intrusion into their realm. The first white man known to travel into the caldera and see the geothermal features was John Colter, who had left the Lewis and Clark Expedition. He described what he saw as "hot spring brimstone". Beaver trapper Joseph Meek recounted in 1830 that the steam rising from the various geyser basins reminded him of smoke coming from industrial smokestacks on a cold winter morning in Pittsburgh, Pennsylvania. In the 1850s famed trapper Jim Bridger called it "the place where Hell bubbled up".

 

The heat that drives geothermal activity in the Yellowstone area comes from brine (salty water) that is 1.5–3 miles (7,900–15,800 ft; 2,400–4,800 m) below the surface. This is actually below the solid volcanic rock and sediment that extends to a depth of 3,000 to 6,000 feet (900 to 1,800 m) and is inside the hot but mostly solid part of the pluton that contains Yellowstone's magma chamber. At that depth the brine is superheated to temperatures that exceed 400 °F (204 °C) but is able to remain a liquid because it is under great pressure (like a huge pressure cooker).

 

Convection of the churning brine and conduction from surrounding rock transfers heat to an overlaying layer of fresh groundwater. Movement of the two liquids is facilitated by the highly fractured and porous nature of the rocks under the Yellowstone Plateau. Some silica is dissolved from the fractured rhyolite into the hot water as it travels through the fractured rock. Part of this hard mineral is later redeposited on the walls of the cracks and fissures to make a nearly pressure-tight system. Silica precipitates at the surface to form either geyserite or sinter, creating the massive geyser cones, the scalloped edges of hot springs, and the seemingly barren landscape of geyser basins.

 

There are at least five types of geothermal features found at Yellowstone:

 

Fumaroles: Fumaroles, or steam vents, are the hottest hydrothermal features in the park. They have so little water that it all flashes into steam before reaching the surface. At places like Roaring Mountain, the result is loud hissing of steam and gases.

Geysers: Geysers such as Old Faithful are a type of geothermal feature that periodically erupt scalding hot water. Increased pressure exerted by the enormous weight of the overlying rock and water prevents deeper water from boiling. As the hot water rises it is under less pressure and steam bubbles form. They, in turn, expand on their ascent until the bubbles are too big and numerous to pass freely through constrictions. At a critical point the confined bubbles actually lift the water above, causing the geyser to splash or overflow. This decreases the pressure of the system and violent boiling results. Large quantities of water flash into tremendous amounts of steam that force a jet of water out of the vent: an eruption begins. Water (and heat) is expelled faster than the geyser's recharge rate, gradually decreasing the system's pressure and eventually ending the eruption.

Hot springs: Hot springs such as Grand Prismatic Spring are the most common hydrothermal features in the park. Their plumbing has no constrictions. Superheated water cools as it reaches the surface, sinks, and is replaced by hotter water from below. This circulation, called convection, prevents water from reaching the temperature needed to set off an eruption. Many hot springs give rise to streams of heated water.

Mudpots: Mudpots such as Fountain Paint Pots are acidic hot springs with a limited water supply. Some microorganisms use hydrogen sulfide (rotten egg smell), which rises from deep within the earth, as an energy source. They convert the gas into sulfuric acid, which breaks down rock into clay.

Travertine terraces: Travertine terraces, found at Mammoth Hot Springs, are formed from limestone (a rock type made of calcium carbonate). Thermal waters rise through the limestone, carrying high amounts of dissolved carbonate. Carbon dioxide is released at the surface and calcium carbonate deposited as travertine, the chalky white rock of the terraces. These features constantly and quickly change due to the rapid rate of deposition.

Geyser basins

 

The Norris Geyser Basin 44°43′43″N 110°42′16″W is the hottest geyser basin in the park and is located near the northwest edge of Yellowstone Caldera near Norris Junction and on the intersection of three major faults. The Norris-Mammoth Corridor is a fault that runs from Norris north through Mammoth to the Gardiner, Montana, area. The Hebgen Lake fault runs from northwest of West Yellowstone, Montana, to Norris. This fault experienced an earthquake in 1959 that measured 7.4 on the Richter scale (sources vary on exact magnitude between 7.1 and 7.8; see 1959 Hebgen Lake earthquake). Norris Geyser Basin is so hot and dynamic because these two faults intersect with the ring fracture zone that resulted from the creation of the Yellowstone Caldera of 640,000 years ago.

 

The Basin consists of three main areas: Porcelain Basin, Back Basin, and One Hundred Springs Plain. Unlike most of other geyser basins in the park, the waters from Norris are acidic rather than alkaline (for example, Echinus Geyser has a pH of ~3.5). The difference in pH allows for a different class of bacterial thermophiles to live at Norris, creating different color patterns in and around the Norris Basin waters.

 

The Ragged Hills that lie between Back Basin and One Hundred Springs Plain are thermally altered glacial kames. As glaciers receded the underlying thermal features began to express themselves once again, melting remnants of the ice and causing masses of debris to be dumped. These debris piles were then altered by steam and hot water flowing through them. Madison lies within the eroded stream channels cut through lava flows formed after the caldera eruption. The Gibbon Falls lies on the caldera boundary as does Virginia Cascades.

 

Algae on left bacteria on right at the intersection of flows from the Constant & Whirlgig Geysers at Norris Geyser Basin

The tallest active geyser in the world, Steamboat Geyser,[11] is located in Norris Basin. Unlike the slightly smaller but much more famous Old Faithful Geyser located in Upper Geyser Basin, Steamboat has an erratic and lengthy timetable between major eruptions. During major eruptions, which may be separated by intervals of more than a year (the longest recorded span between major eruptions was 50 years), Steamboat erupts over 300 feet (90 m) into the air. Steamboat does not lie dormant between eruptions, instead displaying minor eruptions of approximately 40 feet (12 m).

 

Norris Geyser Basin periodically undergoes a large-scale, basin-wide thermal disturbance lasting a few weeks. Water levels fluctuate, and temperatures, pH, colors, and eruptive patterns change throughout the basin. During a disturbance in 1985, Porkchop Geyser continually jetted steam and water; in 1989, the same geyser apparently clogged with silica and blew up, throwing rocks more than 200 feet (61 m). In 2003 a park ranger observed it bubbling heavily, the first such activity seen since 1991. Activity increased dramatically in mid-2003. Because of high ground temperatures and new features beside the trail much of Back Basin was closed until October. In 2004 the boardwalk was routed around the dangerous area and now leads behind Porkchop Geyser.

 

North of Norris, Roaring Mountain is a large, acidic hydrothermal area (solfatara) with many fumaroles. In the late 19th and early 20th centuries, the number, size, and power of the fumaroles were much greater than today. The fumaroles are most easily seen in the cooler, low-light conditions of morning and evening.

 

The Gibbon Geyser Basin 44°41′58″N 110°44′34″W includes several thermal areas in the vicinity of the Gibbon River between Gibbon Falls and Norris. The most accessible feature in the basin is Beryl Spring, with a small boardwalk right along the Grand Loop Road. Artists' Paintpots is a small hydrothermal area south of Norris Junction that includes colorful hot springs and two large mudpots.

 

The Monument Geyser Basin 44°41′03″N 110°45′14″W has no active geysers, but its 'monuments' are siliceous sinter deposits similar to the siliceous spires discovered on the floor of Yellowstone Lake. Scientists hypothesize that this basin's structures formed from a hot water system in a glacially dammed lake during the waning stages of the Pinedale Glaciation. The basin is on a ridge reached by a very steep one-mile (1.6 km) trail south of Artists' Paint Pots. Other areas of thermal activity in Gibbon Geyser Basin lie off-trail.

 

South of Norris along the rim of the caldera is the Upper Geyser Basin 44°27′52″N 110°49′45″W, which has the highest concentration of geothermal features in the park. This complement of features includes the most famous geyser in the park, Old Faithful Geyser, as well as four other predictable large geysers. One of these large geysers in the area is Castle Geyser which is about 1,400 feet (430 m) northwest of Old Faithful. Castle Geyser has an interval of approximately 13 hours between major eruptions, but is unpredictable after minor eruptions. The other three predictable geysers are Grand Geyser, Daisy Geyser, and Riverside Geyser. Biscuit Basin and Black Sand Basin are also within the boundaries of Upper Geyser Basin.

 

The hills surrounding Old Faithful and the Upper Geyser Basin are reminders of Quaternary rhyolitic lava flows. These flows, occurring long after the catastrophic eruption of 640,000 years ago, flowed across the landscape like stiff mounds of bread dough due to their high silica content.

 

Evidence of glacial activity is common, and it is one of the keys that allows geysers to exist. Glacier till deposits underlie the geyser basins providing storage areas for the water used in eruptions. Many landforms, such as Porcupine Hills north of Fountain Flats, are made up of glacial gravel and are reminders that 70,000 to 14,000 years ago, this area was buried under ice.

 

Signs of the forces of erosion can be seen everywhere, from runoff channels carved across the sinter in the geyser basins to the drainage created by the Firehole River. Mountain building is evident on the drive south of Old Faithful, toward Craig Pass. Here the Rocky Mountains reach a height of 8,262 feet (2,518 m), dividing the country into two distinct watersheds.

 

Midway Geyser Basin 44°31′04″N 110°49′56″W is much smaller than the other basins found alongside the Firehole River. Despite its small size, it contains two large features, the 200-by-300-foot-wide (60 by 90 m) Excelsior Geyser which pours over 4,000 U.S. gallons (15,000 L; 3,300 imp gal) per minute into the Firehole River. The largest hot spring in Yellowstone, the 370-foot-wide (110 m) and 121-foot-deep (37 m) Grand Prismatic Spring is found here. Also in the basin is Turquoise Pool and Opal Pool.

 

Lower Geyser Basin

Blue spring with steam rising from it; irregular blotches of red and orange residue are on the banks, along with dead tree trunks.

Silex Spring at Fountain Paint Pot

 

Farther north is the Lower Geyser Basin 44°32′58″N 110°50′09″W, which is the largest geyser basin in area, covering approximately 11 square miles. Due to its large size, it has a much less concentrated set of geothermal features, including Fountain Paint Pots. Fountain Paint Pots are mud pots, that is, a hot spring that contains boiling mud instead of water. The mud is produced by a higher acidity in the water which enables the spring to dissolve surrounding minerals to create an opaque, usually grey, mud. Also there is Firehole Spring, Celestine Pool, Leather Pool, Red Spouter, Jelly spring, and a number of fumaroles.

 

Geysers in Lower Geyser Basin include Great Fountain Geyser, whose eruptions reach 100 to 200 feet (30–61 m) in the air, while waves of water cascade down its sinter terraces., the Fountain group of Geysers (Clepsydra Geyser which erupts nearly continuously to heights of 45 feet (14 m), Fountain Geyser, Jelly Geyser, Jet Geyser, Morning Geyser, and Spasm Geyser), the Pink Cone group of geysers (Dilemma Geyser, Labial Geyser, Narcissus Geyser, Pink Geyser, and Pink Cone Geyser), the White Dome group of geysers (Crack Geyser, Gemini Geyser, Pebble Geyser, Rejuvenated Geyser, and White Dome Geyser), as well as Sizzler Geyser.

 

Clepsydra Geyser erupting. July 2019

Fountain Paint Pots

White Dome Geyser

West Thumb Geyser Basin

Several pools of blue water in ashen rock basin.

West Thumb Geyser Basin

Blackened basin with orange streaks; steam is rising from it with fir trees in the background.

Overflow areas of Silex springs

 

The West Thumb Geyser Basin 44°25′07″N 110°34′23″W, including Potts Basin to the north, is the largest geyser basin on the shores of Yellowstone Lake. The heat source of the thermal features in this location is thought to be relatively close to the surface, only 10,000 feet (3,000 m) down. West Thumb is about the same size as another famous volcanic caldera, Crater Lake in Oregon, but much smaller than the great Yellowstone Caldera which last erupted about 640,000 years ago. West Thumb is a caldera within a caldera.

 

West Thumb was created approximately 162,000 years ago when a magma chamber bulged up under the surface of the earth and subsequently cracked it along ring fracture zones. This in turn released the enclosed magma as lava and caused the surface above the emptied magma chamber to collapse. Water later filled the collapsed area of the caldera, forming an extension of Yellowstone Lake. This created the source of heat and water that feed the West Thumb Geyser Basin today.

 

The thermal features at West Thumb are not only found on the lake shore, but extend under the surface of the lake as well. Several underwater hydrothermal features were discovered in the early 1990s and can be seen as slick spots or slight bulges in the summer. During the winter, the underwater thermal features are visible as melt holes in the icy surface of the lake. The surrounding ice can reach three feet (one yard) in thickness.

 

Perhaps the most famous hydrothermal feature at West Thumb is a geyser on the lake shore known as Fishing Cone. Walter Trumbull of the 1870 Washburn-Langford-Doane Expedition described a unique event while a man was fishing adjacent to the cone: "...in swinging a trout ashore, it accidentally got off the hook and fell into the spring. For a moment it darted about with wonderful rapidity, as if seeking an outlet. Then it came to the top, dead, and literally boiled." Fishing Cone erupted frequently to the height of 40 feet (12 m) in 1919 and to lesser heights in 1939. One fisherman was badly burned in Fishing Cone in 1921. Fishing at the geyser is now prohibited.

 

Early visitors would arrive at West Thumb via stagecoach from the Old Faithful area. They had a choice of continuing on the stagecoach or boarding the steamship Zillah to continue the journey by water to Lake Hotel. The boat dock was located near the south end of the geyser basin near Lakeside Spring.

 

Backcountry Geyser Basins

The Heart Lake 44°18′00″N 110°30′56″W, Lone Star 44°24′50″N 110°49′04″W, and Shoshone Geyser Basins 44°21′16″N 110°47′57″W are located away from the road and require at least several miles of hiking to reach. These areas lack the boardwalks and other safety features of the developed areas. As falling into geothermal features can be fatal, it is usually advisable to visit these areas with an experienced guide or at the very least, travelers need to ensure they remain on well-marked trails.

 

The Heart Lake Geyser Basin contains several groups of geysers and deep blue hot springs near Heart Lake in the south-central portion of Yellowstone, southeast of most of the main geyser basins. Lying in the Snake River watershed east of Lewis Lake and south of Yellowstone Lake, Heart Lake was named sometime before 1871 for Hart Hunney, a hunter. Other explorers in the region incorrectly assumed that the lake's name was spelled 'heart' because of its shape. The Heart Lake Geyser Basin begins a couple miles from the lake and descends along Witch Creek to the lakeshore. Five groups of hydrothermal features comprise the basin, and all of them contain geysers, although some are dormant.

 

Between Shoshone Lake and Old Faithful is the Lone Star Geyser Basin, of which the primary feature is Lone Star Geyser, named for its isolation from the nearby geysers of the Upper Geyser Basin. The basin is reachable on foot or bicycle via a 3 mile road that is closed to vehicles.

 

The Shoshone Geyser Basin, reached by hiking or by boat, contains one of the highest concentrations of geysers in the world – more than 80 in an area 1,600 by 800 feet (490 by 240 m). Hot springs and mudpots dot the landscape between the geyser basin and Shoshone Lake.

 

Hot Spring Basin is located 15 miles (24 km) north-northeast of Fishing Bridge and has one of Yellowstone's largest collections of hot springs and fumaroles. The geothermal features there release large amounts of sulfur. This makes water from the springs so acidic that it has dissolved holes in the pants of people who sit on wet ground and causes mounds of sulfur three feet (1 m) high to develop around fumaroles. The very hot acidic water and steam have also created voids in the ground that are only covered by a thin crust.

 

Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate (over two tons flow into Mammoth each day in a solution). Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas.

 

The thermal features at Mud Volcano and Sulphur Caldron are primarily mud pots and fumaroles because the area is situated on a perched water system with little water available. Fumaroles or "steam vents" occur when the ground water boils away faster than it can be recharged. Also, the vapors are rich in sulfuric acid that leaches the rock, breaking it down into clay. Because no water washes away the acid or leached rock, it remains as sticky clay to form a mud pot. Hydrogen sulfide gas is present deep in the earth at Mud Volcano and is oxidized to sulfuric acid by microbial activity, which dissolves the surface soils to create pools and cones of clay and mud. Along with hydrogen sulfide, steam, carbon dioxide, and other gases explode through the layers of mud.

 

A series of shallow earthquakes associated with the volcanic activity in Yellowstone struck this area in 1978. Soil temperatures increased to nearly 200 °F (93 °C). The slope between Sizzling Basin and Mud Geyser, once covered with green grass and trees, became a barren landscape of fallen trees known as "the cooking hillside".

 

Yellowstone National Park is a national park located in the western United States, largely in the northwest corner of Wyoming and extending into Montana and Idaho. It was established by the 42nd U.S. Congress with the Yellowstone National Park Protection Act and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone was the first national park in the U.S. and is also widely held to be the first national park in the world. The park is known for its wildlife and its many geothermal features, especially the Old Faithful geyser, one of its most popular. While it represents many types of biomes, the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion.

 

While Native Americans have lived in the Yellowstone region for at least 11,000 years, aside from visits by mountain men during the early-to-mid-19th century, organized exploration did not begin until the late 1860s. Management and control of the park originally fell under the jurisdiction of the U.S. Department of the Interior, the first Secretary of the Interior to supervise the park being Columbus Delano. However, the U.S. Army was eventually commissioned to oversee the management of Yellowstone for 30 years between 1886 and 1916. In 1917, the administration of the park was transferred to the National Park Service, which had been created the previous year. Hundreds of structures have been built and are protected for their architectural and historical significance, and researchers have examined more than a thousand archaeological sites.

 

Yellowstone National Park spans an area of 3,468.4 sq mi (8,983 km2), comprising lakes, canyons, rivers, and mountain ranges. Yellowstone Lake is one of the largest high-elevation lakes in North America and is centered over the Yellowstone Caldera, the largest super volcano on the continent. The caldera is considered a dormant volcano. It has erupted with tremendous force several times in the last two million years. Well over half of the world's geysers and hydrothermal features are in Yellowstone, fueled by this ongoing volcanism. Lava flows and rocks from volcanic eruptions cover most of the land area of Yellowstone. The park is the centerpiece of the Greater Yellowstone Ecosystem, the largest remaining nearly intact ecosystem in the Earth's northern temperate zone. In 1978, Yellowstone was named a UNESCO World Heritage Site.

 

Hundreds of species of mammals, birds, fish, reptiles, and amphibians have been documented, including several that are either endangered or threatened. The vast forests and grasslands also include unique species of plants. Yellowstone Park is the largest and most famous megafauna location in the contiguous United States. Grizzly bears, cougars, wolves, and free-ranging herds of bison and elk live in this park. The Yellowstone Park bison herd is the oldest and largest public bison herd in the United States. Forest fires occur in the park each year; in the large forest fires of 1988, nearly one-third of the park was burnt. Yellowstone has numerous recreational opportunities, including hiking, camping, boating, fishing, and sightseeing. Paved roads provide close access to the major geothermal areas as well as some of the lakes and waterfalls. During the winter, visitors often access the park by way of guided tours that use either snow coaches or snowmobiles.

 

Teton County is a county in the U.S. state of Wyoming. As of the 2020 United States Census, the population was 23,331. Its county seat is Jackson. Its west boundary line is also the Wyoming state boundary shared with Idaho and the southern tip of Montana. Teton County is part of the Jackson, WY-ID Micropolitan Statistical Area.

 

Teton County contains the Jackson Hole ski area, all of Grand Teton National Park, and 40.4% of Yellowstone National Park's total area, including over 96.6% of its water area (largely in Yellowstone Lake).

 

Wyoming is a state in the Mountain West subregion of the Western United States. It borders Montana to the north and northwest, South Dakota and Nebraska to the east, Idaho to the west, Utah to the southwest, and Colorado to the south. With a population of 576,851 in 2020, Wyoming is the least populous state despite being the 10th largest by area, with the second-lowest population density after Alaska. The state capital and most populous city is Cheyenne, which had an estimated population of 63,957 in 2018.

 

Wyoming's western half consists mostly of the ranges and rangelands of the Rocky Mountains; its eastern half consists of high-elevation prairie, and is referred to as the High Plains. Wyoming's climate is semi-arid in some parts and continental in others, making it drier and windier overall than other states, with greater temperature extremes. The federal government owns just under half of Wyoming's land, generally protecting it for public uses. The state ranks sixth in the amount of land—-and fifth in the proportion of its land—-that is owned by the federal government. Its federal lands include two national parks (Grand Teton and Yellowstone), two national recreation areas, two national monuments, and several national forests, as well as historic sites, fish hatcheries, and wildlife refuges.

 

Indigenous peoples inhabited the region for thousands of years. Historic and currently federally recognized tribes include the Arapaho, Crow, Lakota, and Shoshone. Part of the land that is now Wyoming came under American sovereignty via the Louisiana Purchase, part via the Oregon Treaty, and, lastly, via the Mexican Cession. With the opening of the Oregon Trail, the Mormon Trail, and the California Trail, vast numbers of pioneers travelled through parts of the state that had once been traversed mainly by fur trappers, and this spurred the establishment of forts, such as Fort Laramie, that today serve as population centers. The Transcontinental Railroad supplanted the wagon trails in 1867 with a route through southern Wyoming, bringing new settlers and the establishment of founding towns, including the state capital of Cheyenne. On March 27, 1890, Wyoming became the union's 44th state.

 

Farming and ranching, and the attendant range wars, feature prominently in the state's history. Today, Wyoming's economy is largely based on tourism and the extraction of minerals such as coal, natural gas, oil, and trona. Its agricultural commodities include barley, hay, livestock, sugar beets, wheat, and wool.

 

Wyoming was the first state to allow women the right to vote (not counting New Jersey, which had allowed it until 1807), and the right to assume elected office, as well as the first state to elect a female governor. In honor of this part of its history, its most common nickname is "The Equality State" and its official state motto is "Equal Rights". It is among the least religious states in the country, and is known for having a political culture that leans towards libertarian conservatism. The Republican presidential nominee has carried the state in every election since 1968.

The red-legged honeycreeper is on average 12.2 cm (4.8 in) long, weighs 14 g (0.49 oz) and has a medium-long black, slightly decurved, bill. The male is violet-blue with black wings, tail and back, and bright red legs. The crown of its head is turquoise, and the underwing, visible only in flight, is lemon yellow. After the breeding season, the male moults into an eclipse plumage, mainly greenish with black wings.

Females and immatures are mainly green, with paler, faintly streaked underparts. The legs are red-brown in the female,

and brown in young birds.

Most of my Costa Rican birds have been photographed at Tico Rainforest B&B. Here, the owner, Victor has documented over 200 different species on his small 2 hectare property. Great place for bird photography.

Best viewed in lightbox - please click on the image or press L.

 

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Spring and fall are the best times of year for sightseeing in Istanbul. The weather is pleasant, with comfortable temperatures averaging around 15°C. While spring is high season in Istanbul, crowds don’t reach their peak until late May. In the fall, the number of tourists who arrive begins to dwindle, with the crowds thinning by early October. Many feel that spring is the best time of all, and particularly April, when the entire city is in bloom for the International Tulip Festival held throughout the month. Still, autumn is the time when the city comes alive in a gamut of colors, both somber and bright, while the light rain and glorious sunsets make for an impressionist painting of sorts. When visiting in the spring, summer or fall, the most pleasant time to experience Istanbul’s top sights is early in the morning, soon after opening, or late in the day. Popular Topkapi Palace is best visited on a Monday morning when it’s usually at its quietest. In winter, you can usually arrive at any time and find no queue or crowds. Summer is just the opposite, arguably the worst time to visit due to the sweltering heat, massive amounts of people visiting the city, and the lines for attractions and other tourist sites. As the major sights in Istanbul all have their own closing days and slightly different operating hours, be sure to check with each one before planning your itinerary.

 

EMIRGAN PARK -

  

The Emirgan Park is a historical urban park located at the Emirgan neighbourhood in the Sarıyer district of Istanbul, Turkey, on the European coast of the Bosphorus. It is one of the largest public parks in Istanbul.

 

In the Byzantine era, the entire area, where today the park stretches, was covered with cypress trees and known as "Kyparades" or "Cypress Forest". It became known as "Feridun Bey Park", when the uninhabited land was granted in the mid-16th century to Nişancı Feridun Bey, a Lord Chancellor in rank in the Ottoman Empire.

 

In the 17th century, Ottoman sultan Murad IV (reigned 1623-1640) presented the estate to Emir Gûne Han, a Safavid Persian commander, who surrendered his sieged castle without any resistance, and followed him back to Istanbul. The name "Feridun Bey Park" was changed to "Emirgûne", which in time became corrupted to "Emirgan".

During the centuries, the estate's owner changed several times, and by the end of the 1860s, it was owned by Khedive Ismail Pasha (reigned 1863-1879), Ottoman governor of Egypt and Sudan. The area was used as the backyard of a large wooden yalı that he built on the shore of the Bosphorus. Further, he built within the park area three wooden pavilions, which still exist.

The heirs of the Khedive's family sold the estate in the 1930s to Satvet Lütfi Tozan, a wealthy Turkish arms dealer, who granted the park grounds, the three pavilions included, later in the 1940s to the City of Istanbul during office of Governor and Mayor Lütfi Kırdar (1938-1949).

 

The park today-

 

A pond with fountain in the Emirgan Park

The park, owned and administered today by the Metropolitan Municipality of Istanbul, covers an area of 117 acres (470,000 m2) on a hillside, and is enclosed by high walls.

Inside the park with two decorative ponds are plants of more than 120 species. The most notable rare trees of the park's flora are: Stone Pine, Turkish pine, Aleppo Pine, Blue Pine, Eastern White Pine, Maritime Pine, Japanese Cedar, Norway Spruce, Blue Spruce, Atlas Cedar, Lebanon Cedar, Himalayan cedar, Beech, Ash tree, Sapindus, Babylon Willow, Hungarian Oak, Colorado White Fir, Maidenhair tree, California incense-cedar, Coast Redwood and Camphor tree.

Many jogging tracks and picnic tables make the Emirgan Park a very popular recreation area for the local people, especially during the weekends and holidays.The three historic pavilions, called after their exterior color as the Yellow Pavilion, the Pink Pavilion and the White Pavilion were restored in time between 1979-1983 by the Touring and Automobile Club of Turkey under its CEO Çelik Gülersoy, and opened to the public as cafeteria and restaurant.

The Emirgan Park is closely associated with the tulip, the traditional flower, which gave its name to an era (1718-1730) of the Ottoman Empire. A special garden was established in Emirgan Park in the 1960s to revive the city's tradition of tulip cultivation. Since 2005, an annual international tulip festival is organized here every April making the park attractive and very colorful with these flowers.

  

The Yellow Pavilion - Sarı Köşk is a large wooden mansion in the form of a chalet built by Khedive Ismail Pasha between 1871-1878 as a hunting lodge and guest house.

Situated in the center of the park and overlooking the Bosphorus, the two-storey mansion with one balcony, one terrace and a basement is constructed on an area of 400 m2 (4,300 sq ft). It consists of four rooms, one hall and a kitchen in the lower floor and three rooms and one salon in the upper floor. Its layout reflects the architecture of the traditional Ottoman house with a salon encircled by many living rooms.

 

The ornaments at the ceilings and the walls were the work of the court architect Sarkis Balyan. The ceilings are enriched with oil painted flower figures and the facades with outstanding carvings. The high doors and windows, as well as the opulent interior decorations in bright colors reflect the glory of that era.

A pond is situated to the northeast, next to the mansion.

Used only by the owners from the very beginning, the pavilion was restored within four months in the beginning of the 1980s with due diligence, furnished with antiques and opened to the public as a cafeteria.The Yellow Pavilion, the main base of the park, is run since 1997 by Beltur, the tourism company of the Metropolitan Municipality of Istanbul. Up to 100 guests can be served at the premise in summer and winter time.

 

The Pink Pavilion - Pembe Köşk, one of the three mansions in the park built by Khedive Ismail Pasha, is a two-storey, typical Ottoman house. Named after its exterior's original color of cranesbill flower pink, the pavilion reflects the glory of its history with fine ornaments.

The pavilion is used as a cafeteria on weekends. Furthermore, it available for conventions and wedding ceremonies. In the summer months, the premise can accommodate up to 350 guests, for cocktails up to 500 people. In the winter time, groups of up to 150 guests can be served.

  

The White Pavilion - Beyaz Köşk is the third mansion within the Emirgan Park built by Khedive Ismail Pasha. It is only 150 m (490 ft) far from the Yellow Pavilion. The two-storey wooden building bears the architectural characteristics of the neo-classical style.

The mansion is used in the daytime as a cafeteria and in the evenings as a restaurant of Turkish-Ottoman cuisine.

  

My sisters and I

The average woman would rather have beauty than brains, because the average man can see better than he can think. ~Author Unknown

 

A chart depicting the average number of calories in an entree salad at various fast food restaurants (McDonald's, Wendy's, Burger King, Chick-fil-A, Taco Bell, Subway, and Arby's)

 

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Gordon.

Like other towns on the Willochra Plains this former wheat farming centre was proclaimed in 1879 following a few years of above average rainfall when the government decided this marginal pastoral land could be opened up for farming. Leasehold land was resumed, surveyed and then put for sale as part of the Hundred of Kanyaka. This was against the advice of the Surveyor General George Goyder who had developed his line of demarcation between farming and pastoral lands back in 1864. The town was named by Governor Jervois after a member of his family which is what he usually did – Amyton, Carrieton, Johnburgh, Hammond, Cradock etc were all named after his family members. He named it after his brother Gordon. The town was near Wirreanda Creek and when the Great Northern Railway came through here in 1880 the station as named Wirreanda! Within a year or so the town had 25 buildings, mainly in stone including the Gordon Hotel, a general store, blacksmith, baker and Bible Christian Methodist Church which was a weatherboard structure only. The state school was completed in 1881 and Catholic Church was built after soon after in 1884. This Catholic Church was replaced with a stone one in 1894. It closed around 1943. The Post Office began in one of the two general stores. Within a few years the rainfall reverted to its usual pattern and the dreams and hopes of the farmers were dashed. The rain did not follow the plough. Most also ran sheep and they provided some income. In the late 1880s locusts and then rabbits destroyed what crops tried farmers tried to grow. Many walked off their lands and the Willochra Plains were soon scattered with deserted stone homesteads. No evidence of them remains today. The school closed in 1928 after several temporary earlier closures and as the former farming properties were amalgamated some stayed on as graziers. When the school closed the hotel was still trading and the two churches were open for worship but the hotel was struggling to survive. It continued into the 1930s and a major town wedding in the Catholic Church took place in 1937 followed by a wedding reception in the Gordon Hotel. It might have been the last event in the hotel which closed in 1942. In 1947 the Gordon Hotel building of 16 main rooms was put up for sale. No buyers came forth and the stone was used to build a new hospital in Quorn. The Methodist Church closed around 1929 and was sold in 1930. Those who were not buried in the Gordon cemetery left the town in the 1930s although the last resident (the Post Mistress) stayed on until 1957. The last burial in the cemetery was in 1969. Today all that can be seen are some piles of rubble and some headstones in the distant cemetery.

 

One of the many old town homes

 

Visby is a popular vacation destination for Scandinavians during the summer and receives thousands of tourists every year. It is by far the most populated locality outside the Swedish mainland. Visby is also the only municipality seat of Sweden that is accessible only by boat and air traffic. The University of Gotland is in Visby, and since 1 July 2013, it is a department of Uppsala University under the name Uppsala university–Campus Gotland.

A chart depicting the average number of calories in a medium milkshake at various fast food restaurants (McDonald's, Wendy's, Burger King, Chick-fil-A, and Arby's)

 

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I average about 6 miles a day (~12k steps) of walking while in the USA because I make a conscious effort to do so.

 

In Tokyo, I'm *easily* making 8+ miles a day just getting around via public transport.

 

Picture I took a few nights back of my Garmin Fenix3 watch showing 22k+ steps (~12mi/19km) done at that point as I was making my way from Agave to a restaurant that Chizuko was waiting for me at.

 

Surprisingly this was not a record for me (record was last year when I was in Tokyo (~24k steps).

 

Ikejiri-Ohashi, Tokyo, Japan.

...complete the Jack Nicolson line ; )

 

Project 52 Flower Power

 

HBW!

Completely average sized truck.

 

Built for Andromeda's Gates on Eurobricks.

In the early seventies, Miranda introduced the Auto Sensorex EE, which in addition to shutter priority auto exposure also featured a switchable spot and averaging light meter. The averaging pattern is the standard Miranda bottom weighted pattern with some minor tweaks; for the spot meter a second round cell was added right in the center, corresponding to the split image rangefinder spot on the screen. This was an ideal location for the spot meter, but the slits in this area of the mirror are visible in the rangefinder spot and take a little getting used to.

These photos are dedicated to the delicacy and beauty of friendships and the sharing of our visions. Since becoming involved with Flickr, I've had the pleasure of getting to know people from different parts of the world. Some of you quite well, and some as casual contacts. Being retired, I probably spend more time on Flickr than the average person. But when I see new images posted by my friends, it always makes me feel better.

 

Several recent posts have been quite thought provoking. I probably write too much in some of my comments, but I just can't help myself. I hope you don't mind. I value these friendships more than words can express.

  

I hope you have a wonderful day!

Hong Kong Tramways (Chinese: 香港電車) is a tram system in Hong Kong and one of the earliest forms of public transport in the metropolis. Owned and operated by Veolia Transport RATP Asia, the tramway runs on Hong Kong Island between Shau Kei Wan and Kennedy Town, with a branch circulating through Happy Valley.

 

Trams in Hong Kong have not only been a form of commuter transport for over 110 years, but also a major tourist attraction and one of the most environmentally friendly ways of travelling in Hong Kong. The tram system is the only one in the world operated exclusively with double-decker trams, and is one of only three non-heritage tram systems in the world that use double-deck cars.

 

The tram is the cheapest mode of public transport on the island. The comparatively affordable fare is highlighted by Hong Kong Tramways' advertising slogan: "Hop on 1. $2.3. Tram so easy!"

 

HISTORY

Hong Kong's tram system was inaugurated using electric trams. It has never used horse or steam power.

 

TIMELINE

1881: Tramway system is proposed for Hong Kong.

1901: Proposal is accepted by Hong Kong Government.

1902: Hong Kong Tramway Electric Company Limited founded.

1902: Name changed to Electric Traction Company of Hong Kong Limited.

1903: Construction of a single-track system began, from Kennedy Town to Causeway Bay. The route was later extended to Shau Kei Wan.

1904: Bodies of the first fleet of 26 tramcars were built in the United Kingdom. They were then shipped in pieces Hung Hom to be assembled. The tramcars were all single-deck. Ten tramcars were designed for first class passengers and the others were for third class passengers. The first-class compartment was enclosed in the centre with two long benches on both sides, with both the front and back ends open. Seating capacity was 32 passengers. The third-class tramcars were open-sided, with six sets of benches running crossways, back to back, seating 48 passengers. Tram fares for the first and the third class were 10 cents and 5 cents respectively. Initially, the company planned to divide the trams into 3 classes, but subsequently only first and third class were chosen for ease of operation.

1910: Name of the company changed to The Hong Kong Tramway Company Limited.

1912: Owing to strong passenger demand, the first double-deck tramcar was introduced in 1912. The tramcar had an open top design, fitted with garden-type seats. The first class occupied the upper deck and one-third of the lower deck. Ten new tramcars were constructed.

1922: Electricity was contracted and supplied by Hong Kong Electric Co. Ltd (HEC). Company name changed to Hong Kong Tramways Limited.

1925: Enclosed double-decker trams replaced open-top trams.

1932: North Point Depot came into service.

1941: Japanese Occupation took place. Very limited tram service was provided. Only 12 tramcars were in operation daily from Causeway Bay to Western Market. One single-decker tram was used as freight transport.

1945: After three years and eight months of Japanese Occupation, all 109 tramcars still remained, but only 15 were operational. By October 1945, 40 tramcars were back in service.

1949: Single-track system was replaced by double-track system in August.

1950: Tramways undertook an extensive re-design and started building its own trams. Tram bodies adopted a "modern" design.

1954: North Point Depot closed and Russell Street Depot expanded and renamed Sharp Street Depot.

1964: Three locally made trams added, including the first single-deck trailer.

1965: Due to passenger demand, 10 single-deck trailers was introduced. The trailer was attached to the back of ordinary tramcar and designed to serve first class passengers only. The maximum capacity was 36 persons for each trailer.

1966: As trailers were well accepted by passengers, 22 single deck trailers were deployed in the fleet during 1966–67. Although trailers played a significant role in the tramways, they were finally withdrawn from the service in 1982.

1967: The last trailer built by the company.

1972: Class distinction abolished and flat fare introduced.

1974: The Hong Kong Tramways Limited acquired by Wharf Holdings

1976 – Drop-in coin boxes were installed on trams. A coin-box was fitted at the front exit, near the driver. Passengers had to drop in the exact fare on leaving the tram. Rotating turnstiles were fitted at the entrance, which is located at the rear of a tram. Conductors were no longer needed and most of them retrained to become motormen.

1986: Tram refurbishment has begun.

1989: Sharp Street Depot closed and terminus function split between Sai Wan Ho and the Whitty Street depots.

1992: Two double-deck trams made by Tramways were exported to the Wirral Tramway, Birkenhead, in the UK.

1992: Point Automation System deployed and points man system for altering the direction of tram manually was abolished.

2000: Coloured destination blinds had begun.

2000: Tramways launched the new "Millennium" tram on 24 October 2000, which was designed and manufactured by its own engineering team. The success of this tramcar marked an important milestone in the history of Hong Kong Tramways.

2001: The Octopus electronic smart card payment system introduced on trams.

2004: Hong Kong Tramways celebrates 100 years of service.

2007: Route map was re-installed on each tram stop. New driving panels were introduced in November.

2008: Air-conditioning was installed on antique tram #128.

2009: 50% stake and operating rights obtained by Veolia Transport RATP Asia; followed by full ownership by Veolia Transport RATP Asia.

2011: Hong Kong Tramways launched the seventh-generation tram on November 28, 2011. It is a combination of modern interior design with traditional tram body exterior. The face-lift allows tram’s iconic image to be maintained.

2014: Hong Kong Tramways celebrates 110 years of service.

2015: Following the opening of the West Island Line, daily tramway ridership drops 10% to 180,000.

 

OWNERSHIP

Hong Kong Tramway Electric Company Limited 1904-1974

The Wharf (Holdings) 1974-2009; retained 50% stake from 2009 to 2010

Veolia Transport RATP Asia 2010–present

 

TRAM ROUTES

The trams run on a double track tramline built parallel to the northern coastline of Hong Kong Island from Kennedy Town to Shau Kei Wan, with a single clockwise-running track of about 3 km around the Happy Valley Racecourse.

 

There are 7 tram termini located along the tram line, namely, from west to east, Kennedy Town, Shek Tong Tsui (a.k.a. Whitty Street), Sheung Wan (Western Market), Happy Valley, Causeway Bay, North Point and Shau Kei Wan; some intermediate stops such as Sai Ying Pun, Admiralty MTR Station, Wan Chai, and Victoria Park are also equipped with crossovers so that they can be used as makeshift termini in emergency situations, such as en-route traffic accidents.

 

There are seven major overlapping routes:

 

Shau Kei Wan ↔ Western Market

Shau Kei Wan ↔ Happy Valley

Shau Kei Wan ↔ Kennedy Town

North Point ↔ Whitty Street

Happy Valley ↔ Kennedy Town

Causeway Bay ↔ Whitty Street

Western Market ↔ Kennedy Town

 

PRACTICAL INFORMATION

Total length – 13 km (with a total track length of 30 km)

Operating Hours – 5:30 am to 12:30 am

Fare – HKD 2.3

 

On average, the headway between each tram departure is approximately 1.5 minutes during peak hours. In the past, trams had a maximum speed of 40 km/h. However, since early 2008, the maximum speed of some trams was increased, with a maximum speed of 50 km/h now enabled on most trams - a few of them even have a maximum speed of 60 km/h. The maximum capacity of each tramcar is 115 people.

 

TICKETS

The current fare is HK$2.30 for adults, HK$1.20 for children under 12, and HK$1.10 for senior citizens 65 and above. Unlike most other forms of public transport in Hong Kong, fare charged is uniform regardless of the distance travelled. Monthly tickets are also available at the cost of HK$200, sold at Shek Tong Tsui, Causeway Bay, and North Point Terminus at the end of each month.

 

Passengers pay upon alighting by either depositing the exact fare in coins into the farebox, or by tapping the Octopus card on the processor. The turnstile at the tram entrance and closed circuit television prevent fare evasion by passengers.

 

Ordinary and antique trams are available for private hire. The open-balcony antique trams are often used for parties and promotional events. Tourists can also travel on the open-top trams through tours organised by the Hong Kong Tourism Board.

 

FLEET

Hong Kong Tramways now owns 163 double axle double-decker trams, including two open-balcony dim-sum tourist trams (Vehicle numbers 28 and 128) for tourist trips and private hire. There are three maintenance-only trams (Vehicle numbers 200, 300 and 400) which operate after tram service has stopped.

 

The trams themselves are sometimes called the "Ding Ding" (Chinese: 叮叮) by Hong Kong people, being the onomatopoeia of the iconic double bell ring trams use to warn pedestrians of their approach. The term "ding ding" is now often used to refer to the whole tram system, e.g. "travel by tram" (Chinese: 搭電車) as "take ding ding" (搭叮叮).

 

Hong Kong has the only fully double-decker tram fleet in the world. Most of the trams in operation were rebodied between 1987 to 1992. They are equipped with sliding windows. Since the early 2000s, these trams have been upgraded to provide better operating performance and safety. Almost all trams have full-body advertisements.

 

FLEET HISTORY

The tram fleet first consisted of 26 single-deck trams, with bodies 8.8 m long and 1.9 m wide, imported from England. However, they were quickly removed because of the rapid modernisation programmes. These tramcars were replaced by open-top double-deck tramcars from 1912 onwards. The introduction of permanent roofs for trams in 1923 was a big improvement to the system. In 1960s, adding trailers was proposed due to the increasing population and demands. In 1964, after testing a prototype built by Taikoo Dockyard in Hong Kong, 10 trailers were ordered from the UK and were added to the trams in Hong Kong in early 1965. Ten additional trailers were ordered from England in 1967, bringing the total number of trailers to 22. They were all withdrawn and scrapped by the end of 1982, since they used to derail frequently and were not economical to run – requiring a separate conductor for only 36 extra passengers.

 

Trams 12 and 50 are the only two trams still maintaining the original 1950s design, being restored at a railway museum in the United States and at a museum in Hong Kong, respectively. The cabins are varnished with their original light-green colour with teak-lined windows and rattan seats.

In 2000, three new aluminium alloy metal-bodied trams (officially called "Millennium trams"), #168 – 170, started operation. These trams have proven quite unpopular due to the poor ventilation in the summer – unlike on previous models, the front screen window cannot be opened to improve air-flow to passengers. A prototype air-conditioned tram, number 171, is under testing.

 

In 2007, a new maintenance tram was constructed, number 300, which is used to move trams in the depot. Besides electric power, it also uses a diesel motor.

 

Starting 7 November, new driving panels has been installed on trams after refurbishment. The first tram on the program was number 38.

 

In 2008, an air-conditioner was installed on the 'antique' tram #128.

Tram RefurbishmentIn October 2010, Veolia Transport showcased a prototype for the new model of trams. It plans to renovate the whole fleet at a cost of HKD 75 Million. The trams would keep their original exterior design, but the outer structure would be aluminium rather than teak as it is more durable. The benches on the lower deck would be replaced with single seats as well as a more modern look. Digital broadcasts would be placed inside trams to inform passengers of the next station, and LED lighting will be installed. AC motors and a new eddy current emergency braking system would be installed.

 

ALIGNMENT AND INTERCHANGES

In many places, trams shares route along with other vehicles.

 

Most of the tram stop locations have remained unchanged since their establishment. However, some have had their names changed, e.g. "Shu Shun Kwun" (Chinese 書信館), referring to the then General Post Office building in the 1940s, is now called "Pedder Street" - the GPO building was demolished in the 1970s, and World-Wide House now stands on its site. In 1934, Hong Kong Tramways introduced loading islands (waiting areas) at some busy tram stops to ensure the safety of passengers. Today, there are 123 tram stops in total, most of them are sheltered refuge islands.

 

Just like buses, trams in Hong Kong can be very crowded. During the busier periods of the day, trams often line up since there are many tramcars running at the same time. In 2002, the trams recorded an average of 240,000 passenger trips daily.

 

Tram stops are densely located in an average interval of 250 metres. Most of them are located in the middle of the road, connected by pedestrian crossings or footbridges. Major stops include Yee Wo Street stop at Causeway Bay, Pacific Place stop at Admiralty, and Prince's Building / The Landmark stop at Central.

 

Many termini of the Hong Kong Tramways are in the form of balloon loops, enabling the trams to reverse its travel direction efficiently.

 

The Island Line of the MTR is roughly parallel to the tramway line between Kennedy Town and Shau Kei Wan stations. Some sections of MTR tunnels are built directly under roads with tram tracks.

 

PUBLIC RECEPTION AND CULTURAL SIGNIFICANCE

The trams have not only been a form of transportation for over a century, but also a major tourist attraction. The well-preserved tram lines still serve as a crucial means of transport in Hong Kong. Travelling in the lower deck of the tram allows travellers to have a close up view of the local street life, while occupying the front seats of the upper deck gives good views of the town as the tram rattles by.

 

Hong Kong's tram system is an icon of the city, like other Asian trams in Kolkata, Dalian and Sapporo.

 

As they run through the urban area of Hong Kong Island, the tram tracks have become an important icon of urban Hong Kong. Since the tracks were originally built along the waterfront before further land reclamation pushed the coastline northwards, the tracks can be used to identify directions and locations throughout urban Hong Kong Island.

 

RED LIGHT MEALS

In the old days, the duration of meal breaks allocated to tram drivers were far from adequate. Most drivers would therefore take advantage of the time their trams are waiting at a red light to gulp down a portion of their meal before the signal turns to green, continuing this practice whenever the tram comes to a red light until the meal is finished. This kind of hurried, impromptu meal is commonly referred as "red light meals" (Chinese: 紅燈飯).

 

PROJECTS

MODERN TRAMWAY AT KAI TAK DEVELOPMENT

Hong Kong Tramways Limited announced its interest in constructing a 12-km modern tramway system in the Kai Tak Development, built on the vacated site of the former Kai Tak Airport, in place of the "Environmentally Friendly Linkage System" (monorail system) proposed by the Hong Kong Government. Possible extensions to neighbouring places such as To Kwa Wan, Kowloon City and Kwun Tong were suggested. The company appointed a consultancy firm to investigate on the feasibility of building such a modern tram system in 2010, and submitted a proposal to the Development Bureau on April 29, 2013.

 

The company pointed out that the cost of constructing the proposed tram system is HK$2.8 billion. which is comparatively low as compared to the cost of $12 billion needed for a monorail system. Bruno Charrade, Managing Director of HKT, said the design of tramcars can be in connection with their Hong Kong Island counterparts or in a totally new shape, depending on the Government's discretion.

 

ABANDONED EXTENSIONS

There have previously been two separate extensions planned that were subsequently modified to be developed as light rail and metro systems.

 

NEW TERRITORIES REAM SYSTEM

During the development of Tuen Mun New Town in the 1970s, the Government had reserved space for the construction of a rail transportation system to serve the area. In 1982, the Government invited the Hong Kong Tramways to construct and operate a tram system in the area. The company initially expressed interest in the construction of the railway and intended to operate with double-decker trams, but later withdrew. The government then invited KCRC to construct and operate a light rail way. The system opened to the public on 18 September 1988. Since 2007, it is now known as the Light Rail.

 

CHAI WAN LINE

In 1970, Chai Wan on eastern Hong Kong Island was developed into a residential and industrial area, which greatly increased the traffic demand to Central. Extending the tram line from Shau Kei Wan to Chai Wan was considered, but was ultimately rejected due to low cost-effectiveness, as hills exist between Chai Wan and Shau Kei Wan, and difficulties arise from tunneling through the hills to make level track. It was replaced by the Island Line service - linking Chai Wan and Admiralty - which was opened to the public on 31 May 1985.

 

WIKIPEDIA

Average 3 inches tall diecast figures from Marvel and Star Wars universe by Takara Tomy in 2016. Hulk, Thor, Captain America, Spider-Man and Star Wars series #16 C-3PO. I forgot to include some more new arrivals. Later…

"Society Hill is a historic neighborhood in Center City Philadelphia, with a population of 6,215 as of the 2010 United States Census. Settled in the early 1680s, Society Hill is one of the oldest residential neighborhoods in Philadelphia. After urban decay developed between the late 19th and early 20th centuries, an urban renewal program began in the 1950s, restoring the area and its many historic buildings. Society Hill has since become one of the most expensive neighborhoods with the highest average income and second-highest real estate values in Philadelphia. Society Hill's historic colonial architecture, along with planning and restoration efforts, led the American Planning Association to designate it, in 2008, as one of the great American neighborhoods and a good example of sustainable urban living.

 

The neighborhood hosts one of the largest concentrations of original 18th- and early 19th-century buildings in the United States. Society Hill is noted for its Franklin street lamps, brick sidewalks, cobblestone and Belgian block streets bordered by two- to four-story brick rowhouses in Federal and Georgian architecture, and public buildings in Greek Revival architecture such as the Merchants' Exchange Building and the Old Pine Street Church.

 

Philadelphia, often called Philly, is the largest city in the Commonwealth of Pennsylvania, the sixth-largest city in the U.S., the second-largest city in both the Northeast megalopolis and Mid-Atlantic regions after New York City, and the 68th-largest city in the world. Since 1854, the city has been coextensive with Philadelphia County, the most populous county in Pennsylvania and the urban core of the Delaware Valley, the nation's seventh-largest and world's 68th-largest metropolitan region, with 6.245 million residents as of 2020. The city's population as of the 2020 census was 1,603,797, and over 56 million people live within 250 mi (400 km) of Philadelphia.

 

Philadelphia was founded in 1682 by William Penn, an English Quaker. The city served as capital of the Pennsylvania Colony during the British colonial era and went on to play a historic and vital role as the central meeting place for the nation's founding fathers whose plans and actions in Philadelphia ultimately inspired the American Revolution and the nation's independence. Philadelphia hosted the First Continental Congress in 1774 following the Boston Tea Party, preserved the Liberty Bell, and hosted the Second Continental Congress during which the founders signed the Declaration of Independence, which historian Joseph Ellis has described as "the most potent and consequential words in American history". Once the Revolutionary War commenced, both the Battle of Germantown and the Siege of Fort Mifflin were fought within Philadelphia's city limits. The U.S. Constitution was later ratified in Philadelphia at the Philadelphia Convention of 1787. Philadelphia remained the nation's largest city until 1790, when it was surpassed by New York City, and served as the nation's first capital from May 10, 1775, until December 12, 1776, and on four subsequent occasions during and following the American Revolution, including from 1790 to 1800 while the new national capital of Washington, D.C. was under construction.

 

During the 19th and 20th centuries, Philadelphia emerged as a major national industrial center and railroad hub. The city’s blossoming industrial sector attracted European immigrants, predominantly from Germany and Ireland, the two largest reported ancestry groups in the city as of 2015. In the 20th century, immigrant waves from Italy and elsewhere in Southern Europe arrived. Following the end of the Civil War in 1865, Philadelphia became a leading destination for African Americans in the Great Migration. In the 20th century, Puerto Rican Americans moved to the city in large numbers. Between 1890 and 1950, Philadelphia's population doubled to 2.07 million. Philadelphia has since attracted immigrants from East and South Asia, Eastern Europe, and Latin America.

 

With 18 four-year universities and colleges, Philadelphia is one of the nation's leading centers for higher education and academic research. As of 2021, the Philadelphia metropolitan area was the nation's ninth-largest metropolitan economy with a gross metropolitan product (GMP) of US$479 billion. Philadelphia is the largest center of economic activity in Pennsylvania and the broader multi-state Delaware Valley region; the city is home to five Fortune 500 corporate headquarters as of 2022. The Philadelphia skyline, which includes several globally renowned commercial skyscrapers, is expanding, primarily with new residential high-rise condominiums. The city and the Delaware Valley are a biotechnology and venture capital hub; and the Philadelphia Stock Exchange, owned by NASDAQ, is the nation's oldest stock exchange and a global leader in options trading. 30th Street Station, the city's primary rail station, is the third-busiest Amtrak hub in the nation, and the city's multimodal transport and logistics infrastructure, including Philadelphia International Airport, the PhilaPort seaport, freight rail infrastructure, roadway traffic capacity, and warehouse storage space, are all expanding.

 

Philadelphia is a national cultural hub, hosting more outdoor sculptures and murals than any other American city. Fairmount Park, when combined with adjacent Wissahickon Valley Park in the same watershed, is 2,052 acres (830 ha), representing one of the nation's largest contiguous urban parks and the 45th largest urban park in the world. The city is known for its arts, culture, cuisine, and colonial and Revolution-era history; in 2016, it attracted 42 million domestic tourists who spent $6.8 billion, representing $11 billion in total economic impact to the city and surrounding Pennsylvania counties.

 

With five professional sports teams and a hugely loyal fan base, the city is often ranked as the nation's best city for professional sports fans. The city has a culturally and philanthropically active LGBTQ+ community. Philadelphia also has played an immensely influential historic and ongoing role in the development and evolution of American music, especially R&B, soul, and rock.

 

Philadelphia is a city of many firsts, including the nation's first library (1731), hospital (1751), medical school (1765), national capital (1774), university (by some accounts) (1779), stock exchange (1790), zoo (1874), and business school (1881). Philadelphia contains 67 National Historic Landmarks, including Independence Hall. From the city's 17th century founding through the present, Philadelphia has been the birthplace or home to an extensive number of prominent and influential Americans. In 2021, Time magazine named Philadelphia one of the world's greatest 100 places." - info from Wikipedia.

 

The fall of 2022 I did my 3rd major cycling tour. I began my adventure in Montreal, Canada and finished in Savannah, GA. This tour took me through the oldest parts of Quebec and the 13 original US states. During this adventure I cycled 7,126 km over the course of 2.5 months and took more than 68,000 photos. As with my previous tours, a major focus was to photograph historic architecture.

 

Now on Instagram.

 

Become a patron to my photography on Patreon or donate.

The Church of Saint Matthew is a Church of England Grade II* listed church located in the High Elswick area of Newcastle upon Tyne, within the Georgian suburb of Summerhill.

 

History

Saint Matthew's was formed out of Saint John's parish in November, 1869, and the Parish is the home of four former parishes - Saint Philip (Elswick), Saint Augustine (Brighton Grove), Saint Matthew (Big Lamp), and Saint Mary the Virgin (Rye Hill).

 

Tradition

Saint Matthew's was founded after the foundations of the Catholic Revival had been set; with its first Vicar, Father Robert Daunt, being described by the time of his death as "a decided High Churchman, who held strong views on the question of the independence of the Church in spiritual matters.". As such, the church has, from its founding, followed the Anglo-Catholic High Church tradition — a rarity within the diocese.

 

Elswick is a district and electoral ward of the city and metropolitan borough of Newcastle upon Tyne, in the county of Tyne and Wear, England, 1.9 miles west of the city centre, bordering the River Tyne. Historically in Northumberland, Elswick became part of Newcastle upon Tyne in 1835. Elswick is home to the Newcastle Utilita Arena; and Newcastle College, with approximately 45,000 students.

 

History

In Roman times the Vallum, a defensive barrier behind Hadrian's Wall, reached its easternmost limit in Elswick. The Wall itself carried on as far as Wallsend.

 

The township of Elswick had originally formed part of the Barony of Bolam and was owned by Tynemouth Priory from 1120-1539, with a fishery present on the site. One of the earliest references to the coal mining industry of the north east occurs in 1330, when it was recorded that the Prior of Tynemouth let a colliery, called Heygrove, at "Elstewyke" for a rent of £5 per year. Elswick Colliery had 3 pits working from 1860 onwards. Elswick was owned by the Crown from 1539 to 1628, until it was sold by Charles I.

 

The Priors held a mansion in the middle of Elswick which was later occupied by Elswick Hall. Having been rebuilt a number of times, the last rebuild took place in 1810. The grounds of Elswick Hall became Elswick Park in 1881. Elswick changed significantly in the late 19th century with the extension of the railway from Carlisle to Newcastle in 1839 and the establishment of Armstrong's manufacturing works in 1847. Population increased rapidly during this period, from about 300 in 1801 to 59,165 in 1901. Tyneside flats were built in the area around Scotswood Road to accommodate the workforce.

 

The Elswick works was founded in 1847 by engineer William George Armstrong. It manufactured hydraulic machinery, cranes and bridges and, later, artillery. In 1882 the company merged with the shipbuilding firm of Charles Mitchell to form Armstrong, Mitchell & Company. Armstrong Mitchell merged again with the engineering firm of Joseph Whitworth in 1897, forming Armstrong, Whitworth & Co.

 

Elswick railway station was opened in 1889 to serve the area. It was located at the western end of the Elswick Works, whose workforce made up a significant proportion of travellers. The area suffered as a result of the inter-war and subsequent depressions, culminating in the demolition of the Elswick works. The station was closed and then demolished in 1967.

 

Elswick was hit hard by the decline of Tyneside's shipbuilding industry during the second half of the 20th century, and by the 1990s was widely regarded as one of the worst parts of Tyneside, if not the whole of Britain. According to a report by The Independent newspaper, unemployment stood at nearly 30% and the area had a widespread problem with drug abuse and arson attacks.

 

Elswick was formerly a township in the parish of Newcastle-St. John, in 1866 Elswick became a separate civil parish, on 1 April 1914 the parish was abolished to form Newcastle upon Tyne. In 1911 the parish had a population of 58,352. It is now in the unparished area of Newcastle upon Tyne.

 

Elswick today

Present day Elswick consists of a number of distinct neighbourhoods including the Adelaide Terrace area, Bentinck Estate, Condercum and Denhill Park, Cruddas Park (part renamed Riverside Dene), Elswick Triangle, Gill Street and the Courts, Grainger Park, Jubilee Estate, North Benwell, and both from the St John's and St Paul's areas. The local authority ward also incorporates Newcastle College, and the Utilita Arena Newcastle. As of the 2011 census, Elswick had one of the lowest White populations in Newcastle at around 55% with a large Asian population of 33.4% (including 15.9% Bangladeshi, 8.3% Pakistani), and 5.6% Black or Black British. Elswick has a large Muslim population of 31.9% and a Christian population of 43.4%. In 2018 it had an estimated population of 15,869.

 

The ward profile shows Elswick is the ward with the highest percentage of children under 14 years in Newcastle and has a lower than average number of senior citizens (10%) than Newcastle as a whole. Elswick has a lower than average number of houses in owner-occupation (26.3% compared with 49.9% for Newcastle city).

 

Elswick's Location

Located at a height of 53.1m, Elswick overlooks the River Tyne and is a suburban area in the West End of Newcastle upon Tyne.

 

Newcastle upon Tyne, or simply Newcastle is a cathedral city and metropolitan borough in Tyne and Wear, England. It is located on the River Tyne's northern bank, opposite Gateshead to the south. It is the most populous settlement in the Tyneside conurbation and North East England.

 

Newcastle developed around a Roman settlement called Pons Aelius, the settlement became known as Monkchester before taking on the name of a castle built in 1080 by William the Conqueror's eldest son, Robert Curthose. It was one of the world's largest ship building and repair centres during the industrial revolution. Newcastle was part of the county of Northumberland until 1400, when it separated and formed a county of itself. In 1974, Newcastle became part of Tyne and Wear. Since 2018, the city council has been part of the North of Tyne Combined Authority.

 

The history of Newcastle upon Tyne dates back almost 2,000 years, during which it has been controlled by the Romans, the Angles and the Norsemen amongst others. Newcastle upon Tyne was originally known by its Roman name Pons Aelius. The name "Newcastle" has been used since the Norman conquest of England. Due to its prime location on the River Tyne, the town developed greatly during the Middle Ages and it was to play a major role in the Industrial Revolution, being granted city status in 1882. Today, the city is a major retail, commercial and cultural centre.

 

Roman settlement

The history of Newcastle dates from AD 122, when the Romans built the first bridge to cross the River Tyne at that point. The bridge was called Pons Aelius or 'Bridge of Aelius', Aelius being the family name of Roman Emperor Hadrian, who was responsible for the Roman wall built across northern England along the Tyne–Solway gap. Hadrian's Wall ran through present-day Newcastle, with stretches of wall and turrets visible along the West Road, and at a temple in Benwell. Traces of a milecastle were found on Westgate Road, midway between Clayton Street and Grainger Street, and it is likely that the course of the wall corresponded to present-day Westgate Road. The course of the wall can be traced eastwards to the Segedunum Roman fort at Wallsend, with the fort of Arbeia down-river at the mouth of the Tyne, on the south bank in what is now South Shields. The Tyne was then a wider, shallower river at this point and it is thought that the bridge was probably about 700 feet (210 m) long, made of wood and supported on stone piers. It is probable that it was sited near the current Swing Bridge, due to the fact that Roman artefacts were found there during the building of the latter bridge. Hadrian himself probably visited the site in 122. A shrine was set up on the completed bridge in 123 by the 6th Legion, with two altars to Neptune and Oceanus respectively. The two altars were subsequently found in the river and are on display in the Great North Museum in Newcastle.

 

The Romans built a stone-walled fort in 150 to protect the river crossing which was at the foot of the Tyne Gorge, and this took the name of the bridge so that the whole settlement was known as Pons Aelius. The fort was situated on a rocky outcrop overlooking the new bridge, on the site of the present Castle Keep. Pons Aelius is last mentioned in 400, in a Roman document listing all of the Roman military outposts. It is likely that nestling in the shadow of the fort would have been a small vicus, or village. Unfortunately, no buildings have been detected; only a few pieces of flagging. It is clear that there was a Roman cemetery near Clavering Place, behind the Central station, as a number of Roman coffins and sarcophagi have been unearthed there.

 

Despite the presence of the bridge, the settlement of Pons Aelius was not particularly important among the northern Roman settlements. The most important stations were those on the highway of Dere Street running from Eboracum (York) through Corstopitum (Corbridge) and to the lands north of the Wall. Corstopitum, being a major arsenal and supply centre, was much larger and more populous than Pons Aelius.

 

Anglo-Saxon development

The Angles arrived in the North-East of England in about 500 and may have landed on the Tyne. There is no evidence of an Anglo-Saxon settlement on or near the site of Pons Aelius during the Anglo-Saxon age. The bridge probably survived and there may well have been a small village at the northern end, but no evidence survives. At that time the region was dominated by two kingdoms, Bernicia, north of the Tees and ruled from Bamburgh, and Deira, south of the Tees and ruled from York. Bernicia and Deira combined to form the kingdom of Northanhymbra (Northumbria) early in the 7th century. There were three local kings who held the title of Bretwalda – 'Lord of Britain', Edwin of Deira (627–632), Oswald of Bernicia (633–641) and Oswy of Northumbria (641–658). The 7th century became known as the 'Golden Age of Northumbria', when the area was a beacon of culture and learning in Europe. The greatness of this period was based on its generally Christian culture and resulted in the Lindisfarne Gospels amongst other treasures. The Tyne valley was dotted with monasteries, with those at Monkwearmouth, Hexham and Jarrow being the most famous. Bede, who was based at Jarrow, wrote of a royal estate, known as Ad Murum, 'at the Wall', 12 miles (19 km) from the sea. It is thought that this estate may have been in what is now Newcastle. At some unknown time, the site of Newcastle came to be known as Monkchester. The reason for this title is unknown, as we are unaware of any specific monasteries at the site, and Bede made no reference to it. In 875 Halfdan Ragnarsson, the Danish Viking conqueror of York, led an army that attacked and pillaged various monasteries in the area, and it is thought that Monkchester was also pillaged at this time. Little more was heard of it until the coming of the Normans.

 

Norman period

After the arrival of William the Conqueror in England in 1066, the whole of England was quickly subjected to Norman rule. However, in Northumbria there was great resistance to the Normans, and in 1069 the newly appointed Norman Earl of Northumbria, Robert de Comines and 700 of his men were killed by the local population at Durham. The Northumbrians then marched on York, but William was able to suppress the uprising. That same year, a second uprising occurred when a Danish fleet landed in the Humber. The Northumbrians again attacked York and destroyed the garrison there. William was again able to suppress the uprising, but this time he took revenge. He laid waste to the whole of the Midlands and the land from York to the Tees. In 1080, William Walcher, the Norman bishop of Durham and his followers were brutally murdered at Gateshead. This time Odo, bishop of Bayeux, William's half brother, devastated the land between the Tees and the Tweed. This was known as the 'Harrying of the North'. This devastation is reflected in the Domesday Book. The destruction had such an effect that the North remained poor and backward at least until Tudor times and perhaps until the Industrial Revolution. Newcastle suffered in this respect with the rest of the North.

 

In 1080 William sent his eldest son, Robert Curthose, north to defend the kingdom against the Scots. After his campaign, he moved to Monkchester and began the building of a 'New Castle'. This was of the "motte-and-bailey" type of construction, a wooden tower on top of an earthen mound (motte), surrounded by a moat and wooden stockade (bailey). It was this castle that gave Newcastle its name. In 1095 the Earl of Northumbria, Robert de Mowbray, rose up against the king, William Rufus, and Rufus sent an army north to recapture the castle. From then on the castle became crown property and was an important base from which the king could control the northern barons. The Northumbrian earldom was abolished and a Sheriff of Northumberland was appointed to administer the region. In 1091 the parish church of St Nicholas was consecrated on the site of the present Anglican cathedral, close by the bailey of the new castle. The church is believed to have been a wooden building on stone footings.

 

Not a trace of the tower or mound of the motte and bailey castle remains now. Henry II replaced it with a rectangular stone keep, which was built between 1172 and 1177 at a cost of £1,444. A stone bailey, in the form of a triangle, replaced the previous wooden one. The great outer gateway to the castle, called 'the Black Gate', was built later, between 1247 and 1250, in the reign of Henry III. There were at that time no town walls and when attacked by the Scots, the townspeople had to crowd into the bailey for safety. It is probable that the new castle acted as a magnet for local merchants because of the safety it provided. This in turn would help to expand trade in the town. At this time wool, skins and lead were being exported, whilst alum, pepper and ginger were being imported from France and Flanders.

 

Middle Ages

Throughout the Middle Ages, Newcastle was England's northern fortress, the centre for assembled armies. The Border war against Scotland lasted intermittently for several centuries – possibly the longest border war ever waged. During the civil war between Stephen and Matilda, David 1st of Scotland and his son were granted Cumbria and Northumberland respectively, so that for a period from 1139 to 1157, Newcastle was effectively in Scottish hands. It is believed that during this period, King David may have built the church of St Andrew and the Benedictine nunnery in Newcastle. However, King Stephen's successor, Henry II was strong enough to take back the Earldom of Northumbria from Malcolm IV.

 

The Scots king William the Lion was imprisoned in Newcastle, in 1174, after being captured at the Battle of Alnwick. Edward I brought the Stone of Scone and William Wallace south through the town and Newcastle was successfully defended against the Scots three times during the 14th century.

 

Around 1200, stone-faced, clay-filled jetties were starting to project into the river, an indication that trade was increasing in Newcastle. As the Roman roads continued to deteriorate, sea travel was gaining in importance. By 1275 Newcastle was the sixth largest wool exporting port in England. The principal exports at this time were wool, timber, coal, millstones, dairy produce, fish, salt and hides. Much of the developing trade was with the Baltic countries and Germany. Most of the Newcastle merchants were situated near the river, below the Castle. The earliest known charter was dated 1175 in the reign of Henry II, giving the townspeople some control over their town. In 1216 King John granted Newcastle a mayor[8] and also allowed the formation of guilds (known as Mysteries). These were cartels formed within different trades, which restricted trade to guild members. There were initially twelve guilds. Coal was being exported from Newcastle by 1250, and by 1350 the burgesses received a royal licence to export coal. This licence to export coal was jealously guarded by the Newcastle burgesses, and they tried to prevent any one else on the Tyne from exporting coal except through Newcastle. The burgesses similarly tried to prevent fish from being sold anywhere else on the Tyne except Newcastle. This led to conflicts with Gateshead and South Shields.

 

In 1265, the town was granted permission to impose a 'Wall Tax' or Murage, to pay for the construction of a fortified wall to enclose the town and protect it from Scottish invaders. The town walls were not completed until early in the 14th century. They were two miles (3 km) long, 9 feet (2.7 m) thick and 25 feet (7.6 m) high. They had six main gates, as well as some smaller gates, and had 17 towers. The land within the walls was divided almost equally by the Lort Burn, which flowed southwards and joined the Tyne to the east of the Castle. The town began to expand north of the Castle and west of the Lort Burn with various markets being set up within the walls.

 

In 1400 Henry IV granted a new charter, creating a County corporate which separated the town, but not the Castle, from the county of Northumberland and recognised it as a "county of itself" with a right to have a sheriff of its own. The burgesses were now allowed to choose six aldermen who, with the mayor would be justices of the peace. The mayor and sheriff were allowed to hold borough courts in the Guildhall.

 

Religious houses

During the Middle Ages a number of religious houses were established within the walls: the first of these was the Benedictine nunnery of St Bartholomew founded in 1086 near the present-day Nun Street. Both David I of Scotland and Henry I of England were benefactors of the religious house. Nothing of the nunnery remains now.

 

The friary of Blackfriars, Newcastle (Dominican) was established in 1239. These were also known as the Preaching Friars or Shod Friars, because they wore sandals, as opposed to other orders. The friary was situated in the present-day Friars Street. In 1280 the order was granted royal permission to make a postern in the town walls to communicate with their gardens outside the walls. On 19 June 1334, Edward Balliol, claimant to be King of Scotland, did homage to King Edward III, on behalf of the kingdom of Scotland, in the church of the friary. Much of the original buildings of the friary still exist, mainly because, after the Dissolution of the Monasteries the friary of Blackfriars was rented out by the corporation to nine of the local trade guilds.

 

The friary of Whitefriars (Carmelite) was established in 1262. The order was originally housed on the Wall Knoll in Pandon, but in 1307 it took over the buildings of another order, which went out of existence, the Friars of the Sac. The land, which had originally been given by Robert the Bruce, was situated in the present-day Hanover Square, behind the Central station. Nothing of the friary remains now.

 

The friary of Austinfriars (Augustinian) was established in 1290. The friary was on the site where the Holy Jesus Hospital was built in 1682. The friary was traditionally the lodging place of English kings whenever they visited or passed through Newcastle. In 1503 Princess Margaret, eldest daughter of Henry VII of England, stayed two days at the friary on her way to join her new husband James IV of Scotland.

 

The friary of Greyfriars (Franciscans) was established in 1274. The friary was in the present-day area between Pilgrim Street, Grey Street, Market Street and High Chare. Nothing of the original buildings remains.

 

The friary of the Order of the Holy Trinity, also known as the Trinitarians, was established in 1360. The order devoted a third of its income to buying back captives of the Saracens, during the Crusades. Their house was on the Wall Knoll, in Pandon, to the east of the city, but within the walls. Wall Knoll had previously been occupied by the White Friars until they moved to new premises in 1307.

 

All of the above religious houses were closed in about 1540, when Henry VIII dissolved the monasteries.

 

An important street running through Newcastle at the time was Pilgrim Street, running northwards inside the walls and leading to the Pilgrim Gate on the north wall. The street still exists today as arguably Newcastle's main shopping street.

 

Tudor period

The Scottish border wars continued for much of the 16th century, so that during that time, Newcastle was often threatened with invasion by the Scots, but also remained important as a border stronghold against them.

 

During the Reformation begun by Henry VIII in 1536, the five Newcastle friaries and the single nunnery were dissolved and the land was sold to the Corporation and to rich merchants. At this time there were fewer than 60 inmates of the religious houses in Newcastle. The convent of Blackfriars was leased to nine craft guilds to be used as their headquarters. This probably explains why it is the only one of the religious houses whose building survives to the present day. The priories at Tynemouth and Durham were also dissolved, thus ending the long-running rivalry between Newcastle and the church for control of trade on the Tyne. A little later, the property of the nunnery of St Bartholomew and of Grey Friars were bought by Robert Anderson, who had the buildings demolished to build his grand Newe House (also known as Anderson Place).

 

With the gradual decline of the Scottish border wars the town walls were allowed to decline as well as the castle. By 1547, about 10,000 people were living in Newcastle. At the beginning of the 16th century exports of wool from Newcastle were more than twice the value of exports of coal, but during the century coal exports continued to increase.

 

Under Edward VI, John Dudley, Duke of Northumberland, sponsored an act allowing Newcastle to annexe Gateshead as its suburb. The main reason for this was to allow the Newcastle Hostmen, who controlled the export of Tyne coal, to get their hands on the Gateshead coal mines, previously controlled by the Bishop of Durham. However, when Mary I came to power, Dudley met his downfall and the decision was reversed. The Reformation allowed private access to coal mines previously owned by Tynemouth and Durham priories and as a result coal exports increase dramatically, from 15,000 tons in 1500 to 35,000 tons in 1565, and to 400,000 tons in 1625.

 

The plague visited Newcastle four times during the 16th century, in 1579 when 2,000 people died, in 1589 when 1700 died, in 1595 and finally in 1597.

 

In 1600 Elizabeth I granted Newcastle a charter for an exclusive body of electors, the right to elect the mayor and burgesses. The charter also gave the Hostmen exclusive rights to load coal at any point on the Tyne. The Hostmen developed as an exclusive group within the Merchant Adventurers who had been incorporated by a charter in 1547.

 

Stuart period

In 1636 there was a serious outbreak of bubonic plague in Newcastle. There had been several previous outbreaks of the disease over the years, but this was the most serious. It is thought to have arrived from the Netherlands via ships that were trading between the Tyne and that country. It first appeared in the lower part of the town near the docks but gradually spread to all parts of the town. As the disease gained hold the authorities took measures to control it by boarding up any properties that contained infected persons, meaning that whole families were locked up together with the infected family members. Other infected persons were put in huts outside the town walls and left to die. Plague pits were dug next to the town's four churches and outside the town walls to receive the bodies in mass burials. Over the course of the outbreak 5,631 deaths were recorded out of an estimated population of 12,000, a death rate of 47%.

 

In 1637 Charles I tried to raise money by doubling the 'voluntary' tax on coal in return for allowing the Newcastle Hostmen to regulate production and fix prices. This caused outrage amongst the London importers and the East Anglian shippers. Both groups decided to boycott Tyne coal and as a result forced Charles to reverse his decision in 1638.

 

In 1640 during the Second Bishops' War, the Scots successfully invaded Newcastle. The occupying army demanded £850 per day from the Corporation to billet the Scottish troops. Trade from the Tyne ground to a halt during the occupation. The Scots left in 1641 after receiving a Parliamentary pardon and a £4,000,000 loan from the town.

 

In 1642 the English Civil War began. King Charles realised the value of the Tyne coal trade and therefore garrisoned Newcastle. A Royalist was appointed as governor. At that time, Newcastle and King's Lynn were the only important seaports to support the crown. In 1644 Parliament blockaded the Tyne to prevent the king from receiving revenue from the Tyne coal trade. Coal exports fell from 450,000 to 3,000 tons and London suffered a hard winter without fuel. Parliament encouraged the coal trade from the Wear to try to replace that lost from Newcastle but that was not enough to make up for the lost Tyneside tonnage.

 

In 1644 the Scots crossed the border. Newcastle strengthened its defences in preparation. The Scottish army, with 40,000 troops, besieged Newcastle for three months until the garrison of 1,500 surrendered. During the siege, the Scots bombarded the walls with their artillery, situated in Gateshead and Castle Leazes. The Scottish commander threatened to destroy the steeple of St Nicholas's Church by gunfire if the mayor, Sir John Marley, did not surrender the town. The mayor responded by placing Scottish prisoners that they had captured in the steeple, so saving it from destruction. The town walls were finally breached by a combination of artillery and sapping. In gratitude for this defence, Charles gave Newcastle the motto 'Fortiter Defendit Triumphans' to be added to its coat of arms. The Scottish army occupied Northumberland and Durham for two years. The coal taxes had to pay for the Scottish occupation. In 1645 Charles surrendered to the Scots and was imprisoned in Newcastle for nine months. After the Civil War the coal trade on the Tyne soon picked up and exceeded its pre-war levels.

 

A new Guildhall was completed on the Sandhill next to the river in 1655, replacing an earlier facility damaged by fire in 1639, and became the meeting place of Newcastle Town Council. In 1681 the Hospital of the Holy Jesus was built partly on the site of the Austin Friars. The Guildhall and Holy Jesus Hospital still exist.

 

Charles II tried to impose a charter on Newcastle to give the king the right to appoint the mayor, sheriff, recorder and town clerk. Charles died before the charter came into effect. In 1685, James II tried to replace Corporation members with named Catholics. However, James' mandate was suspended in 1689 after the Glorious Revolution welcoming William of Orange. In 1689, after the fall of James II, the people of Newcastle tore down his bronze equestrian statue in Sandhill and tossed it into the Tyne. The bronze was later used to make bells for All Saints Church.

 

In 1689 the Lort Burn was covered over. At this time it was an open sewer. The channel followed by the Lort Burn became the present day Dean Street. At that time, the centre of Newcastle was still the Sandhill area, with many merchants living along the Close or on the Side. The path of the main road through Newcastle ran from the single Tyne bridge, through Sandhill to the Side, a narrow street which climbed steeply on the north-east side of the castle hill until it reached the higher ground alongside St Nicholas' Church. As Newcastle developed, the Side became lined with buildings with projecting upper stories, so that the main street through Newcastle was a narrow, congested, steep thoroughfare.

 

In 1701 the Keelmen's Hospital was built in the Sandgate area of the city, using funds provided by the keelmen. The building still stands today.

 

Eighteenth century

In the 18th century, Newcastle was the country's largest print centre after London, Oxford and Cambridge, and the Literary and Philosophical Society of 1793, with its erudite debates and large stock of books in several languages predated the London Library by half a century.

 

In 1715, during the Jacobite rising in favour of the Old Pretender, an army of Jacobite supporters marched on Newcastle. Many of the Northumbrian gentry joined the rebels. The citizens prepared for its arrival by arresting Jacobite supporters and accepting 700 extra recruits into the local militia. The gates of the city were closed against the rebels. This proved enough to delay an attack until reinforcements arrived forcing the rebel army to move across to the west coast. The rebels finally surrendered at Preston.

 

In 1745, during a second Jacobite rising in favour of the Young Pretender, a Scottish army crossed the border led by Bonnie Prince Charlie. Once again Newcastle prepared by arresting Jacobite supporters and inducting 800 volunteers into the local militia. The town walls were strengthened, most of the gates were blocked up and some 200 cannon were deployed. 20,000 regulars were billeted on the Town Moor. These preparations were enough to force the rebel army to travel south via the west coast. They were eventually defeated at Culloden in 1746.

 

Newcastle's actions during the 1715 rising in resisting the rebels and declaring for George I, in contrast to the rest of the region, is the most likely source of the nickname 'Geordie', applied to people from Tyneside, or more accurately Newcastle. Another theory, however, is that the name 'Geordie' came from the inventor of the Geordie lamp, George Stephenson. It was a type of safety lamp used in mining, but was not invented until 1815. Apparently the term 'German Geordie' was in common use during the 18th century.

 

The city's first hospital, Newcastle Infirmary opened in 1753; it was funded by public subscription. A lying-in hospital was established in Newcastle in 1760. The city's first public hospital for mentally ill patients, Wardens Close Lunatic Hospital was opened in October 1767.

 

In 1771 a flood swept away much of the bridge at Newcastle. The bridge had been built in 1250 and repaired after a flood in 1339. The bridge supported various houses and three towers and an old chapel. A blue stone was placed in the middle of the bridge to mark the boundary between Newcastle and the Palatinate of Durham. A temporary wooden bridge had to be built, and this remained in use until 1781, when a new stone bridge was completed. The new bridge consisted of nine arches. In 1801, because of the pressure of traffic, the bridge had to be widened.

 

A permanent military presence was established in the city with the completion of Fenham Barracks in 1806. The facilities at the Castle for holding assizes, which had been condemned for their inconvenience and unhealthiness, were replaced when the Moot Hall opened in August 1812.

 

Victorian period

Present-day Newcastle owes much of its architecture to the work of the builder Richard Grainger, aided by architects John Dobson, Thomas Oliver, John and Benjamin Green and others. In 1834 Grainger won a competition to produce a new plan for central Newcastle. He put this plan into effect using the above architects as well as architects employed in his own office. Grainger and Oliver had already built Leazes Terrace, Leazes Crescent and Leazes Place between 1829 and 1834. Grainger and Dobson had also built the Royal Arcade at the foot of Pilgrim Street between 1830 and 1832. The most ambitious project covered 12 acres 12 acres (49,000 m2) in central Newcastle, on the site of Newe House (also called Anderson Place). Grainger built three new thoroughfares, Grey Street, Grainger Street and Clayton Street with many connecting streets, as well as the Central Exchange and the Grainger Market. John Wardle and George Walker, working in Grainger's office, designed Clayton Street, Grainger Street and most of Grey Street. Dobson designed the Grainger Market and much of the east side of Grey Street. John and Benjamin Green designed the Theatre Royal at the top of Grey Street, where Grainger placed the column of Grey's Monument as a focus for the whole scheme. Grey Street is considered to be one of the finest streets in the country, with its elegant curve. Unfortunately most of old Eldon Square was demolished in the 1960s in the name of progress. The Royal Arcade met a similar fate.

 

In 1849 a new bridge was built across the river at Newcastle. This was the High Level Bridge, designed by Robert Stephenson, and slightly up river from the existing bridge. The bridge was designed to carry road and rail traffic across the Tyne Gorge on two decks with rail traffic on the upper deck and road traffic on the lower. The new bridge meant that traffic could pass through Newcastle without having to negotiate the steep, narrow Side, as had been necessary for centuries. The bridge was opened by Queen Victoria, who one year later opened the new Central Station, designed by John Dobson. Trains were now able to cross the river, directly into the centre of Newcastle and carry on up to Scotland. The Army Riding School was also completed in 1849.

 

In 1854 a large fire started on the Gateshead quayside and an explosion caused it to spread across the river to the Newcastle quayside. A huge conflagration amongst the narrow alleys, or 'chares', destroyed the homes of 800 families as well as many business premises. The narrow alleys that had been destroyed were replaced by streets containing blocks of modern offices.

 

In 1863 the Town Hall in St Nicholas Square replaced the Guildhall as the meeting place of Newcastle Town Council.

 

In 1876 the low level bridge was replaced by a new bridge known as the Swing Bridge, so called because the bridge was able to swing horizontally on a central axis and allow ships to pass on either side. This meant that for the first time sizeable ships could pass up-river beyond Newcastle. The bridge was built and paid for by William Armstrong, a local arms manufacturer, who needed to have warships access his Elswick arms factory to fit armaments to them. The Swing Bridge's rotating mechanism is adapted from the cannon mounts developed in Armstrong's arms works. In 1882 the Elswick works began to build ships as well as to arm them. The Barrack Road drill hall was completed in 1890.

 

Industrialisation

In the 19th century, shipbuilding and heavy engineering were central to the city's prosperity; and the city was a powerhouse of the Industrial Revolution. Newcastle's development as a major city owed most to its central role in the production and export of coal. The phrase "taking coals to Newcastle" was first recorded in 1538; it proverbially denotes bringing a particular commodity to a place that has more than enough of it already.

 

Innovation in Newcastle and surrounding areas included the following:

 

George Stephenson developed a miner's safety lamp at the same time that Humphry Davy developed a rival design. The lamp made possible the opening up of ever deeper mines to provide the coal that powered the industrial revolution.

George and his son Robert Stephenson were hugely influential figures in the development of the early railways. George developed Blücher, a locomotive working at Killingworth colliery in 1814, whilst Robert was instrumental in the design of Rocket, a revolutionary design that was the forerunner of modern locomotives. Both men were involved in planning and building railway lines, all over this country and abroad.

 

Joseph Swan demonstrated a working electric light bulb about a year before Thomas Edison did the same in the USA. This led to a dispute as to who had actually invented the light bulb. Eventually the two rivals agreed to form a mutual company between them, the Edison and Swan Electric Light Company, known as Ediswan.

 

Charles Algernon Parsons invented the steam turbine, for marine use and for power generation. He used Turbinia, a small, turbine-powered ship, to demonstrate the speed that a steam turbine could generate. Turbinia literally ran rings around the British Fleet at a review at Spithead in 1897.

 

William Armstrong invented a hydraulic crane that was installed in dockyards up and down the country. He then began to design light, accurate field guns for the British army. These were a vast improvement on the existing guns that were then in use.

 

The following major industries developed in Newcastle or its surrounding area:

 

Glassmaking

A small glass industry existed in Newcastle from the mid-15th century. In 1615 restrictions were put on the use of wood for manufacturing glass. It was found that glass could be manufactured using the local coal, and so a glassmaking industry grew up on Tyneside. Huguenot glassmakers came over from France as refugees from persecution and set up glasshouses in the Skinnerburn area of Newcastle. Eventually, glass production moved to the Ouseburn area of Newcastle. In 1684 the Dagnia family, Sephardic Jewish emigrants from Altare, arrived in Newcastle from Stourbridge and established glasshouses along the Close, to manufacture high quality flint glass. The glass manufacturers used sand ballast from the boats arriving in the river as the main raw material. The glassware was then exported in collier brigs. The period from 1730 to 1785 was the highpoint of Newcastle glass manufacture, when the local glassmakers produced the 'Newcastle Light Baluster'. The glassmaking industry still exists in the west end of the city with local Artist and Glassmaker Jane Charles carrying on over four hundred years of hot glass blowing in Newcastle upon Tyne.

 

Locomotive manufacture

In 1823 George Stephenson and his son Robert established the world's first locomotive factory near Forth Street in Newcastle. Here they built locomotives for the Stockton and Darlington Railway and the Liverpool and Manchester Railway, as well as many others. It was here that the famous locomotive Rocket was designed and manufactured in preparation for the Rainhill Trials. Apart from building locomotives for the British market, the Newcastle works also produced locomotives for Europe and America. The Forth Street works continued to build locomotives until 1960.

 

Shipbuilding

In 1296 a wooden, 135 ft (41 m) long galley was constructed at the mouth of the Lort Burn in Newcastle, as part of a twenty-ship order from the king. The ship cost £205, and is the earliest record of shipbuilding in Newcastle. However the rise of the Tyne as a shipbuilding area was due to the need for collier brigs for the coal export trade. These wooden sailing ships were usually built locally, establishing local expertise in building ships. As ships changed from wood to steel, and from sail to steam, the local shipbuilding industry changed to build the new ships. Although shipbuilding was carried out up and down both sides of the river, the two main areas for building ships in Newcastle were Elswick, to the west, and Walker, to the east. By 1800 Tyneside was the third largest producer of ships in Britain. Unfortunately, after the Second World War, lack of modernisation and competition from abroad gradually caused the local industry to decline and die.

 

Armaments

In 1847 William Armstrong established a huge factory in Elswick, west of Newcastle. This was initially used to produce hydraulic cranes but subsequently began also to produce guns for both the army and the navy. After the Swing Bridge was built in 1876 allowing ships to pass up river, warships could have their armaments fitted alongside the Elswick works. Armstrong's company took over its industrial rival, Joseph Whitworth of Manchester in 1897.

 

Steam turbines

Charles Algernon Parsons invented the steam turbine and, in 1889, founded his own company C. A. Parsons and Company in Heaton, Newcastle to make steam turbines. Shortly after this, he realised that steam turbines could be used to propel ships and, in 1897, he founded a second company, Parsons Marine Steam Turbine Company in Wallsend. It is there that he designed and manufactured Turbinia. Parsons turbines were initially used in warships but soon came to be used in merchant and passenger vessels, including the liner Mauretania which held the blue riband for the Atlantic crossing until 1929. Parsons' company in Heaton began to make turbo-generators for power stations and supplied power stations all over the world. The Heaton works, reduced in size, remains as part of the Siemens AG industrial giant.

 

Pottery

In 1762 the Maling pottery was founded in Sunderland by French Huguenots, but transferred to Newcastle in 1817. A factory was built in the Ouseburn area of the city. The factory was rebuilt twice, finally occupying a 14-acre (57,000 m2) site that was claimed to be the biggest pottery in the world and which had its own railway station. The pottery pioneered use of machines in making potteries as opposed to hand production. In the 1890s the company went up-market and employed in-house designers. The period up to the Second World War was the most profitable with a constant stream of new designs being introduced. However, after the war, production gradually declined and the company closed in 1963.

 

Expansion of the city

Newcastle was one of the boroughs reformed by the Municipal Corporations Act 1835: the reformed municipal borough included the parishes of Byker, Elswick, Heaton, Jesmond, Newcastle All Saints, Newcastle St Andrew, Newcastle St John, Newcastle St Nicholas, and Westgate. The urban districts of Benwell and Fenham and Walker were added in 1904. In 1935, Newcastle gained Kenton and parts of the parishes of West Brunton, East Denton, Fawdon, Longbenton. The most recent expansion in Newcastle's boundaries took place under the Local Government Act 1972 on 1 April 1974, when Newcastle became a metropolitan borough, also including the urban districts of Gosforth and Newburn, and the parishes of Brunswick, Dinnington, Hazlerigg, North Gosforth and Woolsington from the Castle Ward Rural District, and the village of Westerhope.

 

Meanwhile Northumberland County Council was formed under the Local Government Act 1888 and benefited from a dedicated meeting place when County Hall was completed in the Castle Garth area of Newcastle in 1910. Following the Local Government Act 1972 County Hall relocated to Morpeth in April 1981.

 

Twentieth century

In 1925 work began on a new high-level road bridge to span the Tyne Gorge between Newcastle and Gateshead. The capacity of the existing High-Level Bridge and Swing Bridge were being strained to the limit, and an additional bridge had been discussed for a long time. The contract was awarded to the Dorman Long Company and the bridge was finally opened by King George V in 1928. The road deck was 84 feet (26 m) above the river and was supported by a 531 feet (162 m) steel arch. The new Tyne Bridge quickly became a symbol for Newcastle and Tyneside, and remains so today.

 

During the Second World War, Newcastle was largely spared the horrors inflicted upon other British cities bombed during the Blitz. Although the armaments factories and shipyards along the River Tyne were targeted by the Luftwaffe, they largely escaped unscathed. Manors goods yard and railway terminal, to the east of the city centre, and the suburbs of Jesmond and Heaton suffered bombing during 1941. There were 141 deaths and 587 injuries, a relatively small figure compared to the casualties in other industrial centres of Britain.

 

In 1963 the city gained its own university, the University of Newcastle upon Tyne, by act of parliament. A School of Medicine and Surgery had been established in Newcastle in 1834. This eventually developed into a college of medicine attached to Durham University. A college of physical science was also founded and became Armstrong College in 1904. In 1934 the two colleges merged to become King's College, Durham. This remained as part of Durham University until the new university was created in 1963. In 1992 the city gained its second university when Newcastle Polytechnic was granted university status as Northumbria University.

 

Newcastle City Council moved to the new Newcastle Civic Centre in 1968.

 

As heavy industries declined in the second half of the 20th century, large sections of the city centre were demolished along with many areas of slum housing. The leading political figure in the city during the 1960s was T. Dan Smith who oversaw a massive building programme of highrise housing estates and authorised the demolition of a quarter of the Georgian Grainger Town to make way for Eldon Square Shopping Centre. Smith's control in Newcastle collapsed when it was exposed that he had used public contracts to advantage himself and his business associates and for a time Newcastle became a byword for civic corruption as depicted in the films Get Carter and Stormy Monday and in the television series Our Friends in the North. However, much of the historic Grainger Town area survived and was, for the most part, fully restored in the late 1990s. Northumberland Street, initially the A1, was gradually closed to traffic from the 1970s and completely pedestrianised by 1998.

 

In 1978 a new rapid transport system, the Metro, was built, linking the Tyneside area. The system opened in August 1980. A new bridge was built to carry the Metro across the river between Gateshead and Newcastle. This was the Queen Elizabeth II Bridge, commonly known as the Metro Bridge. Eventually the Metro system was extended to reach Newcastle Airport in 1991, and in 2002 the Metro system was extended to the nearby city of Sunderland.

 

As the 20th century progressed, trade on the Newcastle and Gateshead quaysides gradually declined, until by the 1980s both sides of the river were looking rather derelict. Shipping company offices had closed along with offices of firms related to shipping. There were also derelict warehouses lining the riverbank. Local government produced a master plan to re-develop the Newcastle quayside and this was begun in the 1990s. New offices, restaurants, bars and residential accommodation were built and the area has changed in the space of a few years into a vibrant area, partially returning the focus of Newcastle to the riverside, where it was in medieval times.

 

The Gateshead Millennium Bridge, a foot and cycle bridge, 26 feet (7.9 m) wide and 413 feet (126 m) long, was completed in 2001. The road deck is in the form of a curve and is supported by a steel arch. To allow ships to pass, the whole structure, both arch and road-deck, rotates on huge bearings at either end so that the road deck is lifted. The bridge can be said to open and shut like a human eye. It is an important addition to the re-developed quayside area, providing a vital link between the Newcastle and Gateshead quaysides.

 

Recent developments

Today the city is a vibrant centre for office and retail employment, but just a short distance away there are impoverished inner-city housing estates, in areas originally built to provide affordable housing for employees of the shipyards and other heavy industries that lined the River Tyne. In the 2010s Newcastle City Council began implementing plans to regenerate these depressed areas, such as those along the Ouseburn Valley.

CFF160 refractor, Takahashi 1.5 extender, QHY163M camera. Seeing average.

Arches National Park is a national park in eastern Utah, United States. The park is adjacent to the Colorado River, 4 miles (6 km) north of Moab, Utah. More than 2,000 natural sandstone arches are located in the park, including the well-known Delicate Arch, as well as a variety of unique geological resources and formations. The park contains the highest density of natural arches in the world.

 

The park consists of 310.31 square kilometres (76,680 acres; 119.81 sq mi; 31,031 ha) of high desert located on the Colorado Plateau. The highest elevation in the park is 5,653 feet (1,723 m) at Elephant Butte, and the lowest elevation is 4,085 feet (1,245 m) at the visitor center. The park receives an average of less than 10 inches (250 mm) of rain annually.

 

Administered by the National Park Service, the area was originally named a national monument on April 12, 1929, and was re designated as a national park on November 12, 1971. The park received more than 1.6 million visitors in 2018.

 

As stated in the foundation document in U.S. National Park Service website:

 

The purpose of Arches National Park is to protect extraordinary examples of geologic features including arches, natural bridges, windows, spires, and balanced rocks, as well as other features of geologic, historic, and scientific interest, and to provide opportunities to experience these resources and their associated values in their majestic natural settings.

 

The national park lies above an underground evaporite layer or salt bed, which is the main cause of the formation of the arches, spires, balanced rocks, sandstone fins, and eroded monoliths in the area. This salt bed is thousands of feet thick in places and was deposited in the Paradox Basin of the Colorado Plateau some 300 million years ago (Mya) when a sea flowed into the region and eventually evaporated. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 200 Mya), desert conditions prevailed in the region and the vast Navajo Sandstone was deposited. An additional sequence of stream laid and windblown sediments, the Entrada Sandstone (about 140 Mya), was deposited on top of the Navajo. Over 5,000 feet (1,500 m) of younger sediments were deposited and have been mostly eroded. Remnants of the cover exist in the area including exposures of the Cretaceous Mancos Shale. The arches of the area are developed mostly within the Entrada formation.

 

The weight of this cover caused the salt bed below it to liquefy and thrust up layers of rock into salt domes. The evaporites of the area formed more unusual "salt anticlines" or linear regions of uplift. Faulting occurred and whole sections of rock subsided into the areas between the domes. In some places, they turned almost on edge. The result of one such 2,500-foot (760 m) displacement, the Moab Fault, is seen from the visitor center.

 

As this subsurface movement of salt shaped the landscape, erosion removed the younger rock layers from the surface. Except for isolated remnants, the major formations visible in the park today are the salmon-colored Entrada Sandstone, in which most of the arches form, and the buff-colored Navajo Sandstone. These are visible in layer-cake fashion throughout most of the park. Over time, water seeped into the surface cracks, joints, and folds of these layers. Ice formed in the fissures, expanding and putting pressure on surrounding rock, breaking off bits and pieces. Winds later cleaned out the loose particles. A series of free-standing fins remained. Wind and water attacked these fins until, in some, the cementing material gave way and chunks of rock tumbled out. Many damaged fins collapsed. Others, with the right degree of hardness and balance, survived despite their missing sections. These became the famous arches.

 

Although the park's terrain may appear rugged and durable, it is extremely fragile. More than 1 million visitors each year threaten the fragile high-desert ecosystem. The problem lies within the soil's crust, which is composed of cyanobacteria, algae, fungi, and lichens that grow in the dusty parts of the park. Factors that make Arches National Park sensitive to visitor damage include being a semiarid region, the scarce, unpredictable rainfall, lack of deep freezing, and lack of plant litter, which results in soils that have both a low resistance to and slow recovery from, compressional forces such as foot traffic. Methods of indicating effects on the soil are cytophobic soil crust index, measuring of water infiltration, and t-tests that are used to compare the values from the undisturbed and disturbed areas.

 

Geological processes that occurred over 300 million years ago caused a salt bed to be deposited, which today lies beneath the landscape of Arches National Park.[ Over time, the salt bed was covered with sediments that eventually compressed into rock layers that have since been named Entrada Standstone. Rock layers surrounding the edge of the salt bed continued to erode and shift into vertical sandstone walls called fins. Sand collected between vertical walls of the fins, then slightly acidic rain combined with carbon dioxide in the air allowed for the chemical formation of carbonic acid within the trapped sand. Over time, the carbonic acid dissolved the calcium carbonate that held the sandstone together. Many of the rock formations have weaker layers of rock on bottom that are holding stronger layers on top. The weaker layers would dissolve first, creating openings in the rock. Gravity caused pieces of the stronger rock layer to fall piece by piece into an arch shape. Arches form within rock fins at points of intense fracturing localization, or weak points in the rock's formation, caused by horizontal and vertical discontinuities. Lastly, water, wind, and time continued this erosion process and ultimately created the arches of Arches National Park. All of the arches in the park are made of Entrada Sandstone, however, there are slight differences in how each arch was developed. This allows the Entrada Sandstone to be categories into 3 groups including Slick rock members, Dewey rock members, and Moab members. Vertical arches can be developed from Slick rock members, a combination of Slick rock members and Moab members, or Slick rock members resting above Dewey rock members. Horizontal arches (also called potholes) are formed when a vertical pothole formation meets a horizontal cave, causing a union into a long arch structure. The erosion process within Arches National Park will continue as time continues to pass. Continued erosion combined with vertical and horizontal stress will eventually cause arches to collapse, but still, new arches will continue to form for thousands of years.

 

Humans have occupied the region since the last ice age 10,000 years ago. Fremont people and Ancestral Puebloans lived in the area until about 700 years ago. Spanish missionaries encountered Ute and Paiute tribes in the area when they first came through in 1775, but the first European-Americans to attempt settlement in the area were the Mormon Elk Mountain Mission in 1855, who soon abandoned the area. Ranchers, farmers, and prospectors later settled Moab in the neighboring Riverine Valley in the late 1870s. Word of the beauty of the surrounding rock formations spread beyond the settlement as a possible tourist destination.

 

The Arches area was first brought to the attention of the National Park Service by Frank A. Wadleigh, passenger traffic manager of the Denver and Rio Grande Western Railroad. Wadleigh, accompanied by railroad photographer George L. Beam, visited the area in September 1923 at the invitation of Alexander Ringhoffer, a Hungarian-born prospector living in Salt Valley. Ringhoffer had written to the railroad to interest them in the tourist potential of a scenic area he had discovered the previous year with his two sons and a son-in-law, which he called the Devils Garden (known today as the Klondike Bluffs). Wadleigh was impressed by what Ringhoffer showed him, and suggested to Park Service director Stephen T. Mather that the area be made a national monument.

 

The following year, additional support for the monument idea came from Laurence Gould, a University of Michigan graduate student (and future polar explorer) studying the geology of the nearby La Sal Mountains, who was shown the scenic area by local physician Dr. J. W. "Doc" Williams.

 

A succession of government investigators examined the area, in part due to confusion as to the precise location. In the process, the name Devils Garden was transposed to an area on the opposite side of Salt Valley that includes Landscape Arch, the longest arch in the park. Ringhoffer's original discovery was omitted, while another area nearby, known locally as the Windows, was included. Designation of the area as a national monument was supported by the Park Service in 1926 but was resisted by President Calvin Coolidge's Interior Secretary, Hubert Work. Finally, in April 1929, shortly after his inauguration, President Herbert Hoover signed a presidential proclamation creating the Arches National Monument, consisting of two comparatively small, disconnected sections. The purpose of the reservation under the 1906 Antiquities Act was to protect the arches, spires, balanced rocks, and other sandstone formations for their scientific and educational value. The name Arches was suggested by Frank Pinkely, superintendent of the Park Service's southwestern national monuments, following a visit to the Windows section in 1925.

 

In late 1938, President Franklin D. Roosevelt signed a proclamation that enlarged the Arches to protect additional scenic features and permit the development of facilities to promote tourism. A small adjustment was made by President Dwight Eisenhower in 1960 to accommodate a new road alignment.

 

In early 1969, just before leaving office, President Lyndon B. Johnson signed a proclamation substantially enlarging the Arches. Two years later, President Richard Nixon signed legislation enacted by Congress, which significantly reduced the total area enclosed, but changed its status. Arches National Park was formally dedicated in May 1972.

 

In 1980, vandals attempted to use an abrasive kitchen cleanser to deface ancient petroglyphs in the park, prompting park officials to recruit physicist John F. Asmus, who specialized in using lasers to restore works of art, to use his technology to repair the damage. Asmus "zapped the panel with intense light pulses and succeeded in removing most of the cleanser".

 

Climbing Balanced Rock or any named or unnamed arch in Arches National Park with an opening larger than 3 ft (0.9 m) is banned by park regulations. Climbing on other features in the park is allowed but regulated; in addition, slacklining and BASE jumping are banned parkwide.

 

Climbing on named arches within the park had long been banned by park regulations, but following Dean Potter's successful free climb on Delicate Arch in May 2006, the wording of the regulations was deemed unenforceable by the park attorney. In response, the park revised its regulations later that month, eventually imposing the current ban on arch climbing in 2014.

 

Approved recreational activities include auto touring, hiking, bicycling, camping at the Devils Garden campground, backpacking, canyoneering, and rock climbing, with permits required for the last three activities. Guided commercial tours and ranger programs are also available.

 

Astronomy is also popular in the park due to its dark skies, despite the increasing light pollution from towns such as Moab.

 

Delicate Arch is the subject of the third 2014 quarter of the U.S. Mint's America the Beautiful Quarters program commemorating national parks and historic sites. The Arches quarter had the highest production of the five 2014 national park quarters, with more than 465 million minted.

 

American writer Edward Abbey was a park ranger at Arches National Monument in 1956 and 1957, where he kept journals that became his book Desert Solitaire. The success of Abbey's book, as well as interest in adventure travel, has drawn many hikers, mountain bikers, and off-pavement driving enthusiasts to the area. Permitted activities within the park include camping, hiking along designated trails, backpacking, canyoneering, rock climbing, bicycling, and driving along existing roads, both paved and unpaved. The Hayduke Trail, an 812 mi (1,307 km) backpacking route named after one of Edward Abbey's characters, begins in the park.

 

An abundance of wildlife occurs in Arches National Park, including spadefoot toads, antelope squirrels, scrub jays, peregrine falcons, many kinds of sparrows, red foxes, desert bighorn sheep, kangaroo rats, mule deers, cougars, midget faded rattlesnakes, yucca moths, western rattlesnakes, and collared lizards.

 

A number of plant species are common in the park, including prickly pear cactus, Indian ricegrass, bunch grasses, cheatgrass, moss, liverworts, Utah juniper, Mormon tea, blackbrush, cliffrose, four-winged saltbrush, pinyon pine, evening primrose, sand verbena, yucca, and sacred datura.

 

Biological soil crust consisting of cyanobacteria, lichen, mosses, green algae, and microfungi is found throughout southeastern Utah. The fibrous growths help keep soil particles together, creating a layer that is more resistant to erosion. The living soil layer readily absorbs and stores water, allowing more complex forms of plant life to grow in places with low precipitation levels.

 

Among the notable features of the park are the following:

Balanced Rock – a large balancing rock, the size of three school buses

Courthouse Towers – a collection of tall stone columns

Dark Angel – a free-standing 150 ft-tall (46 m) sandstone pillar at the end of the Devils Garden Trail

Delicate Arch – a lone-standing arch that has become a symbol of Utah and the most recognized arch in the park

Devils Garden – many arches and columns scattered along a ridge

Double Arch – two arches that share a common end

Fiery Furnace – an area of maze-like narrow passages and tall rock columns (see biblical reference, Book of Daniel, chapter 3)

Landscape Arch – a very thin and long arch in the Devils Garden with a span of 290 ft (88 m) (the longest arch in the park)

Petrified Dunes – petrified remnants of dunes blown from the ancient lakes that covered the area

The Phallus – a rock spire that resembles a phallus

Wall Arch – located along the popular Devils Garden Trail; collapsed sometime on August 4/5, 2008

The Three Gossips –a mid-sized sandstone tower located in the Courthouse Towers area.

 

Utah is a landlocked state in the Mountain West subregion of the Western United States. It borders Colorado to its east, Wyoming to its northeast, Idaho to its north, Arizona to its south, and Nevada to its west. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.

 

Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo, and Ute. The Spanish were the first Europeans to arrive in the mid-16th century, though the region's difficult geography and harsh climate made it a peripheral part of New Spain and later Mexico. Even while it was Mexican territory, many of Utah's earliest settlers were American, particularly Mormons fleeing marginalization and persecution from the United States via the Mormon Trail. Following the Mexican–American War in 1848, the region was annexed by the U.S., becoming part of the Utah Territory, which included what is now Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah's admission as a state; only after the outlawing of polygamy was it admitted in 1896 as the 45th.

 

People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. A 2023 paper challenged this perception (claiming only 42% of Utahns are Mormons) however most statistics still show a majority of Utah residents belong to the LDS church; estimates from the LDS church suggests 60.68% of Utah's population belongs to the church whilst some sources put the number as high as 68%. The paper replied that membership count done by the LDS Church is too high for several reasons. The LDS Church greatly influences Utahn culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.

 

Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. Utah ranks among the overall best states in metrics such as healthcare, governance, education, and infrastructure. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah's water security and impacting the state's economy.

 

The History of Utah is an examination of the human history and social activity within the state of Utah located in the western United States.

 

Archaeological evidence dates the earliest habitation of humans in Utah to about 10,000 to 12,000 years ago. Paleolithic people lived near the Great Basin's swamps and marshes, which had an abundance of fish, birds, and small game animals. Big game, including bison, mammoths and ground sloths, also were attracted to these water sources. Over the centuries, the mega-fauna died, this population was replaced by the Desert Archaic people, who sheltered in caves near the Great Salt Lake. Relying more on gathering than the previous Utah residents, their diet was mainly composed of cattails and other salt tolerant plants such as pickleweed, burro weed and sedge. Red meat appears to have been more of a luxury, although these people used nets and the atlatl to hunt water fowl, ducks, small animals and antelope. Artifacts include nets woven with plant fibers and rabbit skin, woven sandals, gaming sticks, and animal figures made from split-twigs. About 3,500 years ago, lake levels rose and the population of Desert Archaic people appears to have dramatically decreased. The Great Basin may have been almost unoccupied for 1,000 years.

 

The Fremont culture, named from sites near the Fremont River in Utah, lived in what is now north and western Utah and parts of Nevada, Idaho and Colorado from approximately 600 to 1300 AD. These people lived in areas close to water sources that had been previously occupied by the Desert Archaic people, and may have had some relationship with them. However, their use of new technologies define them as a distinct people. Fremont technologies include:

 

use of the bow and arrow while hunting,

building pithouse shelters,

growing maize and probably beans and squash,

building above ground granaries of adobe or stone,

creating and decorating low-fired pottery ware,

producing art, including jewelry and rock art such as petroglyphs and pictographs.

 

The ancient Puebloan culture, also known as the Anasazi, occupied territory adjacent to the Fremont. The ancestral Puebloan culture centered on the present-day Four Corners area of the Southwest United States, including the San Juan River region of Utah. Archaeologists debate when this distinct culture emerged, but cultural development seems to date from about the common era, about 500 years before the Fremont appeared. It is generally accepted that the cultural peak of these people was around the 1200 CE. Ancient Puebloan culture is known for well constructed pithouses and more elaborate adobe and masonry dwellings. They were excellent craftsmen, producing turquoise jewelry and fine pottery. The Puebloan culture was based on agriculture, and the people created and cultivated fields of maize, beans, and squash and domesticated turkeys. They designed and produced elaborate field terracing and irrigation systems. They also built structures, some known as kivas, apparently designed solely for cultural and religious rituals.

 

These two later cultures were roughly contemporaneous, and appear to have established trading relationships. They also shared enough cultural traits that archaeologists believe the cultures may have common roots in the early American Southwest. However, each remained culturally distinct throughout most of their existence. These two well established cultures appear to have been severely impacted by climatic change and perhaps by the incursion of new people in about 1200 CE. Over the next two centuries, the Fremont and ancient Pueblo people may have moved into the American southwest, finding new homes and farmlands in the river drainages of Arizona, New Mexico and northern Mexico.

 

In about 1200, Shoshonean speaking peoples entered Utah territory from the west. They may have originated in southern California and moved into the desert environment due to population pressure along the coast. They were an upland people with a hunting and gathering lifestyle utilizing roots and seeds, including the pinyon nut. They were also skillful fishermen, created pottery and raised some crops. When they first arrived in Utah, they lived as small family groups with little tribal organization. Four main Shoshonean peoples inhabited Utah country. The Shoshone in the north and northeast, the Gosiutes in the northwest, the Utes in the central and eastern parts of the region and the Southern Paiutes in the southwest. Initially, there seems to have been very little conflict between these groups.

 

In the early 16th century, the San Juan River basin in Utah's southeast also saw a new people, the Díne or Navajo, part of a greater group of plains Athabaskan speakers moved into the Southwest from the Great Plains. In addition to the Navajo, this language group contained people that were later known as Apaches, including the Lipan, Jicarilla, and Mescalero Apaches.

 

Athabaskans were a hunting people who initially followed the bison, and were identified in 16th-century Spanish accounts as "dog nomads". The Athabaskans expanded their range throughout the 17th century, occupying areas the Pueblo peoples had abandoned during prior centuries. The Spanish first specifically mention the "Apachu de Nabajo" (Navaho) in the 1620s, referring to the people in the Chama valley region east of the San Juan River, and north west of Santa Fe. By the 1640s, the term Navaho was applied to these same people. Although the Navajo newcomers established a generally peaceful trading and cultural exchange with the some modern Pueblo peoples to the south, they experienced intermittent warfare with the Shoshonean peoples, particularly the Utes in eastern Utah and western Colorado.

 

At the time of European expansion, beginning with Spanish explorers traveling from Mexico, five distinct native peoples occupied territory within the Utah area: the Northern Shoshone, the Goshute, the Ute, the Paiute and the Navajo.

 

The Spanish explorer Francisco Vázquez de Coronado may have crossed into what is now southern Utah in 1540, when he was seeking the legendary Cíbola.

 

A group led by two Spanish Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the California coast. The expedition traveled as far north as Utah Lake and encountered the native residents. All of what is now Utah was claimed by the Spanish Empire from the 1500s to 1821 as part of New Spain (later as the province Alta California); and subsequently claimed by Mexico from 1821 to 1848. However, Spain and Mexico had little permanent presence in, or control of, the region.

 

Fur trappers (also known as mountain men) including Jim Bridger, explored some regions of Utah in the early 19th century. The city of Provo was named for one such man, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah is named for a brigade leader of the Hudson's Bay Company, Peter Skene Ogden who trapped in the Weber Valley. In 1846, a year before the arrival of members from the Church of Jesus Christ of latter-day Saints, the ill-fated Donner Party crossed through the Salt Lake valley late in the season, deciding not to stay the winter there but to continue forward to California, and beyond.

 

Members of the Church of Jesus Christ of Latter-day Saints, commonly known as Mormon pioneers, first came to the Salt Lake Valley on July 24, 1847. At the time, the U.S. had already captured the Mexican territories of Alta California and New Mexico in the Mexican–American War and planned to keep them, but those territories, including the future state of Utah, officially became United States territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 10, 1848.

 

Upon arrival in the Salt Lake Valley, the Mormon pioneers found no permanent settlement of Indians. Other areas along the Wasatch Range were occupied at the time of settlement by the Northwestern Shoshone and adjacent areas by other bands of Shoshone such as the Gosiute. The Northwestern Shoshone lived in the valleys on the eastern shore of Great Salt Lake and in adjacent mountain valleys. Some years after arriving in the Salt Lake Valley Mormons, who went on to colonize many other areas of what is now Utah, were petitioned by Indians for recompense for land taken. The response of Heber C. Kimball, first counselor to Brigham Young, was that the land belonged to "our Father in Heaven and we expect to plow and plant it." A 1945 Supreme Court decision found that the land had been treated by the United States as public domain; no aboriginal title by the Northwestern Shoshone had been recognized by the United States or extinguished by treaty with the United States.

 

Upon arriving in the Salt Lake Valley, the Mormons had to make a place to live. They created irrigation systems, laid out farms, built houses, churches, and schools. Access to water was crucially important. Almost immediately, Brigham Young set out to identify and claim additional community sites. While it was difficult to find large areas in the Great Basin where water sources were dependable and growing seasons long enough to raise vitally important subsistence crops, satellite communities began to be formed.

 

Shortly after the first company arrived in the Salt Lake Valley in 1847, the community of Bountiful was settled to the north. In 1848, settlers moved into lands purchased from trapper Miles Goodyear in present-day Ogden. In 1849, Tooele and Provo were founded. Also that year, at the invitation of Ute chief Wakara, settlers moved into the Sanpete Valley in central Utah to establish the community of Manti. Fillmore, Utah, intended to be the capital of the new territory, was established in 1851. In 1855, missionary efforts aimed at western native cultures led to outposts in Fort Lemhi, Idaho, Las Vegas, Nevada and Elk Mountain in east-central Utah.

 

The experiences of returning members of the Mormon Battalion were also important in establishing new communities. On their journey west, the Mormon soldiers had identified dependable rivers and fertile river valleys in Colorado, Arizona and southern California. In addition, as the men traveled to rejoin their families in the Salt Lake Valley, they moved through southern Nevada and the eastern segments of southern Utah. Jefferson Hunt, a senior Mormon officer of the Battalion, actively searched for settlement sites, minerals, and other resources. His report encouraged 1851 settlement efforts in Iron County, near present-day Cedar City. These southern explorations eventually led to Mormon settlements in St. George, Utah, Las Vegas and San Bernardino, California, as well as communities in southern Arizona.

 

Prior to establishment of the Oregon and California trails and Mormon settlement, Indians native to the Salt Lake Valley and adjacent areas lived by hunting buffalo and other game, but also gathered grass seed from the bountiful grass of the area as well as roots such as those of the Indian Camas. By the time of settlement, indeed before 1840, the buffalo were gone from the valley, but hunting by settlers and grazing of cattle severely impacted the Indians in the area, and as settlement expanded into nearby river valleys and oases, indigenous tribes experienced increasing difficulty in gathering sufficient food. Brigham Young's counsel was to feed the hungry tribes, and that was done, but it was often not enough. These tensions formed the background to the Bear River massacre committed by California Militia stationed in Salt Lake City during the Civil War. The site of the massacre is just inside Preston, Idaho, but was generally thought to be within Utah at the time.

 

Statehood was petitioned for in 1849-50 using the name Deseret. The proposed State of Deseret would have been quite large, encompassing all of what is now Utah, and portions of Colorado, Idaho, Nevada, Wyoming, Arizona, Oregon, New Mexico and California. The name of Deseret was favored by the LDS leader Brigham Young as a symbol of industry and was derived from a reference in the Book of Mormon. The petition was rejected by Congress and Utah did not become a state until 1896, following the Utah Constitutional Convention of 1895.

 

In 1850, the Utah Territory was created with the Compromise of 1850, and Fillmore (named after President Fillmore) was designated the capital. In 1856, Salt Lake City replaced Fillmore as the territorial capital.

 

The first group of pioneers brought African slaves with them, making Utah the only place in the western United States to have African slavery. Three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with this first group in 1847. The settlers also began to purchase Indian slaves in the well-established Indian slave trade, as well as enslaving Indian prisoners of war. In 1850, 26 slaves were counted in Salt Lake County. Slavery didn't become officially recognized until 1852, when the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners were passed. Slavery was repealed on June 19, 1862, when Congress prohibited slavery in all US territories.

 

Disputes between the Mormon inhabitants and the federal government intensified after the Church of Jesus Christ of Latter-day Saints' practice of polygamy became known. The polygamous practices of the Mormons, which were made public in 1854, would be one of the major reasons Utah was denied statehood until almost 50 years after the Mormons had entered the area.

 

After news of their polygamous practices spread, the members of the LDS Church were quickly viewed by some as un-American and rebellious. In 1857, after news of a possible rebellion spread, President James Buchanan sent troops on the Utah expedition to quell the growing unrest and to replace Brigham Young as territorial governor with Alfred Cumming. The expedition was also known as the Utah War.

 

As fear of invasion grew, Mormon settlers had convinced some Paiute Indians to aid in a Mormon-led attack on 120 immigrants from Arkansas under the guise of Indian aggression. The murder of these settlers became known as the Mountain Meadows massacre. The Mormon leadership had adopted a defensive posture that led to a ban on the selling of grain to outsiders in preparation for an impending war. This chafed pioneers traveling through the region, who were unable to purchase badly needed supplies. A disagreement between some of the Arkansas pioneers and the Mormons in Cedar City led to the secret planning of the massacre by a few Mormon leaders in the area. Some scholars debate the involvement of Brigham Young. Only one man, John D. Lee, was ever convicted of the murders, and he was executed at the massacre site.

 

Express riders had brought the news 1,000 miles from the Missouri River settlements to Salt Lake City within about two weeks of the army's beginning to march west. Fearing the worst as 2,500 troops (roughly 1/3rd of the army then) led by General Albert Sidney Johnston started west, Brigham Young ordered all residents of Salt Lake City and neighboring communities to prepare their homes for burning and evacuate southward to Utah Valley and southern Utah. Young also sent out a few units of the Nauvoo Legion (numbering roughly 8,000–10,000), to delay the army's advance. The majority he sent into the mountains to prepare defenses or south to prepare for a scorched earth retreat. Although some army wagon supply trains were captured and burned and herds of army horses and cattle run off no serious fighting occurred. Starting late and short on supplies, the United States Army camped during the bitter winter of 1857–58 near a burned out Fort Bridger in Wyoming. Through the negotiations between emissary Thomas L. Kane, Young, Cumming and Johnston, control of Utah territory was peacefully transferred to Cumming, who entered an eerily vacant Salt Lake City in the spring of 1858. By agreement with Young, Johnston established the army at Fort Floyd 40 miles away from Salt Lake City, to the southwest.

 

Salt Lake City was the last link of the First Transcontinental Telegraph, between Carson City, Nevada and Omaha, Nebraska completed in October 1861. Brigham Young, who had helped expedite construction, was among the first to send a message, along with Abraham Lincoln and other officials. Soon after the telegraph line was completed, the Deseret Telegraph Company built the Deseret line connecting the settlements in the territory with Salt Lake City and, by extension, the rest of the United States.

 

Because of the American Civil War, federal troops were pulled out of Utah Territory (and their fort auctioned off), leaving the territorial government in federal hands without army backing until General Patrick E. Connor arrived with the 3rd Regiment of California Volunteers in 1862. While in Utah, Connor and his troops soon became discontent with this assignment wanting to head to Virginia where the "real" fighting and glory was occurring. Connor established Fort Douglas just three miles (5 km) east of Salt Lake City and encouraged his bored and often idle soldiers to go out and explore for mineral deposits to bring more non-Mormons into the state. Minerals were discovered in Tooele County, and some miners began to come to the territory. Conner also solved the Shoshone Indian problem in Cache Valley Utah by luring the Shoshone into a midwinter confrontation on January 29, 1863. The armed conflict quickly turned into a rout, discipline among the soldiers broke down, and the Battle of Bear River is today usually referred to by historians as the Bear River Massacre. Between 200 and 400 Shoshone men, women and children were killed, as were 27 soldiers, with over 50 more soldiers wounded or suffering from frostbite.

 

Beginning in 1865, Utah's Black Hawk War developed into the deadliest conflict in the territory's history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and Utah local militia.

 

On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the state, and several influential businessmen made fortunes in the territory.

 

Main article: Latter Day Saint polygamy in the late-19th century

During the 1870s and 1880s, federal laws were passed and federal marshals assigned to enforce the laws against polygamy. In the 1890 Manifesto, the LDS Church leadership dropped its approval of polygamy citing divine revelation. When Utah applied for statehood again in 1895, it was accepted. Statehood was officially granted on January 4, 1896.

 

The Mormon issue made the situation for women the topic of nationwide controversy. In 1870 the Utah Territory, controlled by Mormons, gave women the right to vote. However, in 1887, Congress disenfranchised Utah women with the Edmunds–Tucker Act. In 1867–96, eastern activists promoted women's suffrage in Utah as an experiment, and as a way to eliminate polygamy. They were Presbyterians and other Protestants convinced that Mormonism was a non-Christian cult that grossly mistreated women. The Mormons promoted woman suffrage to counter the negative image of downtrodden Mormon women. With the 1890 Manifesto clearing the way for statehood, in 1895 Utah adopted a constitution restoring the right of women's suffrage. Congress admitted Utah as a state with that constitution in 1896.

 

Though less numerous than other intermountain states at the time, several lynching murders for alleged misdeeds occurred in Utah territory at the hand of vigilantes. Those documented include the following, with their ethnicity or national origin noted in parentheses if it was provided in the source:

 

William Torrington in Carson City (then a part of Utah territory), 1859

Thomas Coleman (Black man) in Salt Lake City, 1866

3 unidentified men at Wahsatch, winter of 1868

A Black man in Uintah, 1869

Charles A. Benson in Logan, 1873

Ah Sing (Chinese man) in Corinne, 1874

Thomas Forrest in St. George, 1880

William Harvey (Black man) in Salt Lake City, 1883

John Murphy in Park City, 1883

George Segal (Japanese man) in Ogden, 1884

Joseph Fisher in Eureka, 1886

Robert Marshall (Black man) in Castle Gate, 1925

Other lynchings in Utah territory include multiple instances of mass murder of Native American children, women, and men by White settlers including the Battle Creek massacre (1849), Provo River Massacre (1850), Nephi massacre (1853), and Circleville Massacre (1866).

 

Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah began to become known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes, and such natural landmarks as Delicate Arch and "the Mittens" of Monument Valley are instantly recognizable to most national residents. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.

 

Beginning in 1939, with the establishment of Alta Ski Area, Utah has become world-renowned for its skiing. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world. Salt Lake City won the bid for the 2002 Winter Olympics in 1995, and this has served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues scattered across the Wasatch Front continue to be used for sporting events. This also spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the re-construction of the freeway system around the city.

 

During the late 20th century, the state grew quickly. In the 1970s, growth was phenomenal in the suburbs. Sandy was one of the fastest-growing cities in the country at that time, and West Valley City is the state's 2nd most populous city. Today, many areas of Utah are seeing phenomenal growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Transportation and urbanization are major issues in politics as development consumes agricultural land and wilderness areas.

 

In 2012, the State of Utah passed the Utah Transfer of Public Lands Act in an attempt to gain control over a substantial portion of federal land in the state from the federal government, based on language in the Utah Enabling Act of 1894. The State does not intend to use force or assert control by limiting access in an attempt to control the disputed lands, but does intend to use a multi-step process of education, negotiation, legislation, and if necessary, litigation as part of its multi-year effort to gain state or private control over the lands after 2014.

 

Utah families, like most Americans everywhere, did their utmost to assist in the war effort. Tires, meat, butter, sugar, fats, oils, coffee, shoes, boots, gasoline, canned fruits, vegetables, and soups were rationed on a national basis. The school day was shortened and bus routes were reduced to limit the number of resources used stateside and increase what could be sent to soldiers.

 

Geneva Steel was built to increase the steel production for America during World War II. President Franklin D. Roosevelt had proposed opening a steel mill in Utah in 1936, but the idea was shelved after a couple of months. After the attack on Pearl Harbor, the United States entered the war and the steel plant was put into progress. In April 1944, Geneva shipped its first order, which consisted of over 600 tons of steel plate. Geneva Steel also brought thousands of job opportunities to Utah. The positions were hard to fill as many of Utah's men were overseas fighting. Women began working, filling 25 percent of the jobs.

 

As a result of Utah's and Geneva Steels contribution during the war, several Liberty Ships were named in honor of Utah including the USS Joseph Smith, USS Brigham Young, USS Provo, and the USS Peter Skene Ogden.

 

One of the sectors of the beachhead of Normandy Landings was codenamed Utah Beach, and the amphibious landings at the beach were undertaken by United States Army troops.

 

It is estimated that 1,450 soldiers from Utah were killed in the war.

No intoxicants involved. Thinking he’s cool cuz he finally scored in foose-ball

Looks nicer on black, looks very average on white!

 

Took my work lunch break in the sunshine for a change. Spring has properly arrived, and it was really nice just to amble around in the fresh air and see some nice fresh greens that weren't the usual moss on rocks and tree-trunks in the Gelt.

 

I've just finished my presentation and sent it off. Basically, I'm trying to turn this 365 and its stories into a (local interest) book. There's a grant available from a well known non-fiction writer who lives in Cumbria, to help get such projects off the ground. The panel includes the MD of a Cumbrian publishing company, and the head of the tourist authority. I've sent lots of sample spreads with some of my photos and stories. This is my application (with some obscure local references) : -

 

Personal Statement

 

My book is about Cumbria and about living and working in Cumbria in 2013. My working title is 'Landscape 365: A Year of Cumbrian Adventures with a Camera and a pair of Wellies'. It might not seem, from the title, to be an in-depth study of the county in the modern age. But then again it probably isn't. I want to show the beauty of Cumbria through my photography and ally that to some fascinating stories of its history, with a generous helping of light hearted tales of a man struggling to create something worthwhile alongside a family, a career and propensity towards clumsiness.

 

I have set out to take a photograph daily during the year to show the landscapes that are on my doorstep in North Cumbria. Each day this year I have headed to a Cumbrian location, near or far, to take a photograph and write about where I have been, how this connects to my life and what it means to be lucky enough to have such perfection so close to home. My book would need to be large enough to accommodate 365 photographs and daily reflections, probably in the region of 200 pages.

 

Based in Brampton, I need money for travelling expenses to extend my range more regularly into the Lake District. While that may not seem to amount to much, I have 236 days to go at the time of writing, so have plenty of scope to explore Lakeland further. I am proud of my corner of the county but understand that when marketing anything, Cat Bells will beat Cold Fell. To make my project a reality I also need to replace my photographic filters, which have become victims of overuse and wear during this project.

 

The worst part of my asking for this money is that I know that without it, I will still continue and I will finish what I have started. But the money could allow me to broaden its scope to the point where it encompasses enough of Cumbria’s greatest asset, the Lakes, to turn it from my personal project into a saleable book for lovers of this great county. The award would enable me to make my project the best it can be, to allow it to become something so much greater than the sum of its 365 parts. And for that, I would be truly grateful.

 

Biography

 

I was born in Carlisle in 1977, which makes me 35, I think. Certainly old enough that it takes a while to recall my age, but young and hungry enough to want to make my creative dreams a reality. I only lived in Carlisle for my first 6 months and I can’t remember much from that far back as I spent much of my time drinking. Milk mostly.

 

After 12 childhood years in the Midlands I returned to Cumbria and endured 12 sleepless months living in Newtown, on the Brampton to Longtown road. Sleepless on the account of the herd of Blue Faced Gloucester sheep who resided in the field behind my bedroom, and spent every night coughing more than the inhabitants of a late 19th century TB sanatorium.

 

Moving back to Brampton I spent my teenage years doing regular things. Playing football. Watching football. Worshipping Carlisle United at Brunton Park and wondering how Lord Bragg went from painting his London house in Carlisle’s colours in the 70’s to becoming a celebrity Arsenal fan. Just the usual.

 

After university in Leeds I moved to the North East and worked for ten years as the complaints manager at the now failed bank, Northern Rock. While travelling in France towards the end of its decline, a French waiter once told me it must be the worst job in the world. Not quite, I suppose, but it was interesting even he’d heard of how bad things had become. In recent years I have moved back to Brampton and work as Sales & Marketing manager at my family’s company, Omega Music. I have a beautiful 7 year old daughter who would be the subject of every one of my photographs, if she didn’t run at the sight of my camera.

 

I'll find out if its been a success at the start of June.

 

Average annual temperature. Data from the G-Econ project gecon.yale.edu/

 

Rendered using Matlab and PovRay.

Yuanjiajie covers an area of about 1,200 hectares, with an average altitude of 1,074 meters. It is adjacent to Jinbian Creek in the east and overlooks Yaozizhai in the distance; it overlooks Huangshizhai in the south and is connected to Tianbofu; it is connected to Tianzi Mountain in the west; and it is close to Suoxiyu in the north. It is located in the northern part of Zhangjiajie National Forest Park and is a pearl inlaid in the core scenic area of Wulingyuan. Yuanjiajie is located at the northern foot of Shandaogou. It is a huge and relatively gentle mountain composed mainly of quartzite. It is another scenic spot in Zhangjiajie Park. From the left of Zicaotan in Jinbian Creek, you can go to Yuanjiajie; along the edge of Yuanjiajie Terrace, you can also go down to the Qianli Meeting Point of Jinbian Creek by taking the deserted trail; you can also go to Tianzi Mountain and Yangjiazhai from Yuanjiajie. Yuanjiajie, located at the northern foot of Shadaogou, has Zhangjiajie's representative and world-class karst landforms, and is famous for its sandstone peaks and forests. Yuanjiajie perfectly presents the strange mountains and beautiful waters of Zhangjiajie and is the core attraction of the forest park. The ecological environment of the scenic area is well protected, with lush vegetation, fresh air and great pristine beauty. 袁家界面积约1200公顷，平均海拔1074米，它东邻金鞭溪、远眺鹞子寨；南望黄石寨，连接天波府；西通天子山；北距索溪峪。它位于张家界国家森林公园北部，是镶嵌在武陵源核心景区的一颗明珠。袁家界位于杉刀沟北麓，是以石英岩为主构成的一座巨大而较平缓的山岳。是张家界公园又一处风景集中地。自金鞭溪紫草潭左入杉刀沟可上袁家界；顺袁家界台地边沿，绕荒径小道亦可下至金鞭溪千里相会处；亦可从袁家界去天子山、杨家寨. 位于砂刀沟北麓的袁家界拥有张家界代表性的、世界顶级的喀斯特地貌，以砂岩峰林著称。袁家界堪称完美地呈现了张家界的奇山秀水，是森林公园的核心景点。景区生态环境保护较好，植被繁茂，空气清新，极具原生态之美。

Niagara Falls is a group of three waterfalls at the southern end of Niagara Gorge, spanning the border between the province of Ontario in Canada and the state of New York in the United States. The largest of the three is Horseshoe Falls, which straddles the international border of the two countries. It is also known as the Canadian Falls. The smaller American Falls and Bridal Veil Falls lie within the United States. Bridal Veil Falls is separated from Horseshoe Falls by Goat Island and from American Falls by Luna Island, with both islands situated in New York.

 

Formed by the Niagara River, which drains Lake Erie into Lake Ontario, the combined falls have the highest flow rate of any waterfall in North America that has a vertical drop of more than 50 m (160 ft). During peak daytime tourist hours, more than 168,000 m3 (5.9 million cu ft) of water goes over the crest of the falls every minute. Horseshoe Falls is the most powerful waterfall in North America, as measured by flow rate. Niagara Falls is famed for its beauty and is a valuable source of hydroelectric power. Balancing recreational, commercial, and industrial uses has been a challenge for the stewards of the falls since the 19th century.

 

Niagara Falls is 27 km (17 mi) northwest of Buffalo, New York, and 69 km (43 mi) southeast of Toronto, between the twin cities of Niagara Falls, Ontario, and Niagara Falls, New York. Niagara Falls was formed when glaciers receded at the end of the Wisconsin glaciation (the last ice age), and water from the newly formed Great Lakes carved a path over and through the Niagara Escarpment en route to the Atlantic Ocean.

 

Horseshoe Falls is about 57 m (187 ft) high, while the height of the American Falls varies between 21 and 30 m (69 and 98 ft) because of the presence of giant boulders at its base. The larger Horseshoe Falls is about 790 m (2,590 ft) wide, while the American Falls is 320 m (1,050 ft) wide. The distance between the American extremity of Niagara Falls and the Canadian extremity is 1,039 m (3,409 ft).

 

The peak flow over Horseshoe Falls was recorded at 6,370 m3 (225,000 cu ft) per second. The average annual flow rate is 2,400 m3 (85,000 cu ft) per second. Since the flow is a direct function of the Lake Erie water elevation, it typically peaks in late spring or early summer. During the summer months, at least 2,800 m3 (99,000 cu ft) per second of water traverse the falls, some 90% of which goes over Horseshoe Falls, while the balance is diverted to hydroelectric facilities and then on to American Falls and Bridal Veil Falls. This is accomplished by employing a weir – the International Control Dam – with movable gates upstream from Horseshoe Falls.

 

The water flow is halved at night and during the low tourist season winter months and only attains a minimum flow of 1,400 cubic metres (49,000 cu ft) per second. Water diversion is regulated by the 1950 Niagara Treaty and is administered by the International Niagara Board of Control. The verdant green color of the water flowing over Niagara Falls is a byproduct of the estimated 60 tonnes/minute of dissolved salts and rock flour (very finely ground rock) generated by the erosive force of the Niagara River.

 

The Niagara River is an Important Bird Area due to its impact on Bonaparte's gulls, ring-billed gulls, and herring gulls. Several thousand birds migrate and winter in the surrounding area.

 

The features that became Niagara Falls were created by the Wisconsin glaciation about 10,000 years ago. The retreat of the ice sheet left behind a large amount of meltwater (see Lake Algonquin, Lake Chicago, Glacial Lake Iroquois, and Champlain Sea) that filled up the basins that the glaciers had carved, thus creating the Great Lakes as we know them today. Scientists posit there is an old valley, St David's Buried Gorge, buried by glacial drift, at the approximate location of the present Welland Canal.

 

When the ice melted, the upper Great Lakes emptied into the Niagara River, which followed the rearranged topography across the Niagara Escarpment. In time, the river cut a gorge through the north-facing cliff, or cuesta. Because of the interactions of three major rock formations, the rocky bed did not erode evenly. The caprock formation is composed of hard, erosion-resistant limestone and dolomite of the Lockport Formation (Middle Silurian). That hard layer of stone eroded more slowly than the underlying materials. Immediately below the caprock lies the weaker, softer, sloping Rochester Formation (Lower Silurian). This formation is composed mainly of shale, though it has some thin limestone layers. It also contains ancient fossils. In time, the river eroded the soft layer that supported the hard layers, undercutting the hard caprock, which gave way in great chunks. This process repeated countless times, eventually carving out the falls. Submerged in the river in the lower valley, hidden from view, is the Queenston Formation (Upper Ordovician), which is composed of shales and fine sandstones. All three formations were laid down in an ancient sea, their differences of character deriving from changing conditions within that sea.

 

About 10,900 years ago, the Niagara Falls was between present-day Queenston, Ontario, and Lewiston, New York, but erosion of the crest caused the falls to retreat approximately 6.8 miles (10.9 km) southward. The shape of Horseshoe Falls has changed through the process of erosion, evolving from a small arch to a horseshoe bend to the present day V-shape. Just upstream from the falls' current location, Goat Island splits the course of the Niagara River, resulting in the separation of Horseshoe Falls to the west from the American and Bridal Veil Falls to the east. Engineering has slowed erosion and recession.

 

Future of the falls

The current rate of erosion is approximately 30 centimeters (0.98 feet) per year, down from a historical average of 0.91 m (3.0 ft) per year. At this rate, in about 50,000 years Niagara Falls will have eroded the remaining 32 km (20 mi) to Lake Erie, and the falls will cease to exist.

 

Preservation efforts

In the 1870s, sightseers had limited access to Niagara Falls and often had to pay for a glimpse, and industrialization threatened to carve up Goat Island to further expand commercial development. Other industrial encroachments and lack of public access led to a conservation movement in the U.S. known as Free Niagara, led by such notables as Hudson River School artist Frederic Edwin Church, landscape designer Frederick Law Olmsted, and architect Henry Hobson Richardson. Church approached Lord Dufferin, governor-general of Canada, with a proposal for international discussions on the establishment of a public park.

 

Goat Island was one of the inspirations for the American side of the effort. William Dorsheimer, moved by the scene from the island, brought Olmsted to Buffalo in 1868 to design a city park system, which helped promote Olmsted's career. In 1879, the New York state legislature commissioned Olmsted and James T. Gardner to survey the falls and to create the single most important document in the Niagara preservation movement, a "Special Report on the preservation of Niagara Falls". The report advocated for state purchase, restoration and preservation through public ownership of the scenic lands surrounding Niagara Falls. Restoring the former beauty of the falls was described in the report as a "sacred obligation to mankind". In 1883, New York Governor Grover Cleveland drafted legislation authorizing acquisition of lands for a state reservation at Niagara, and the Niagara Falls Association, a private citizens group founded in 1882, mounted a great letter-writing campaign and petition drive in support of the park. Professor Charles Eliot Norton and Olmsted were among the leaders of the public campaign, while New York Governor Alonzo Cornell opposed.

 

Preservationists' efforts were rewarded on April 30, 1885, when Governor David B. Hill signed legislation creating the Niagara Reservation, New York's first state park. New York State began to purchase land from developers, under the charter of the Niagara Reservation State Park. In the same year, the province of Ontario established the Queen Victoria Niagara Falls Park for the same purpose. On the Canadian side, the Niagara Parks Commission governs land usage along the entire course of the Niagara River, from Lake Erie to Lake Ontario.

 

In 1887, Olmsted and Calvert Vaux issued a supplemental report detailing plans to restore the falls. Their intent was "to restore and conserve the natural surroundings of the Falls of Niagara, rather than to attempt to add anything thereto", and the report anticipated fundamental questions, such as how to provide access without destroying the beauty of the falls, and how to restore natural landscapes damaged by man. They planned a park with scenic roadways, paths and a few shelters designed to protect the landscape while allowing large numbers of visitors to enjoy the falls. Commemorative statues, shops, restaurants, and a 1959 glass and metal observation tower were added later. Preservationists continue to strive to strike a balance between Olmsted's idyllic vision and the realities of administering a popular scenic attraction.

 

Preservation efforts continued well into the 20th century. J. Horace McFarland, the Sierra Club, and the Appalachian Mountain Club persuaded the United States Congress in 1906 to enact legislation to preserve the falls by regulating the waters of the Niagara River. The act sought, in cooperation with the Canadian government, to restrict diversion of water, and a treaty resulted in 1909 that limited the total amount of water diverted from the falls by both nations to approximately 56,000 cubic feet per second (1,600 m3/s). That limitation remained in effect until 1950.

 

Erosion control efforts have always been of importance. Underwater weirs redirect the most damaging currents, and the top of the falls has been strengthened. In June 1969, the Niagara River was completely diverted from American Falls for several months through construction of a temporary rock and earth dam. During this time, two bodies were removed from under the falls, including a man who had been seen jumping over the falls, and the body of a woman, which was discovered once the falls dried. While Horseshoe Falls absorbed the extra flow, the U.S. Army Corps of Engineers studied the riverbed and mechanically bolted and strengthened any faults they found; faults that would, if left untreated, have hastened the retreat of American Falls. A plan to remove the huge mound of talus deposited in 1954 was abandoned owing to cost, and in November 1969, the temporary dam was dynamited, restoring flow to American Falls. Even after these undertakings, Luna Island, the small piece of land between the American Falls and Bridal Veil Falls, remained off limits to the public for years owing to fears that it was unstable and could collapse into the gorge.

 

Commercial interests have continued to encroach on the land surrounding the state park, including the construction of several tall buildings (most of them hotels) on the Canadian side. The result is a significant alteration and urbanisation of the landscape. One study found that the tall buildings changed the breeze patterns and increased the number of mist days from 29 per year to 68 per year, but another study disputed this idea.

 

In 2013, New York State began an effort to renovate Three Sisters Islands located south of Goat Island. Funds were used from the re-licensing of the New York Power Authority hydroelectric plant downriver in Lewiston, New York, to rebuild walking paths on the Three Sisters Islands and to plant native vegetation on the islands. The state also renovated the area around Prospect Point at the brink of American Falls in the state park.

 

Toponymy

Theories differ as to the origin of the name of the falls. The Native American word Ongiara means thundering water; The New York Times used this in 1925. According to Iroquoian scholar Bruce Trigger, Niagara is derived from the name given to a branch of the local native Neutral Confederacy, who are described as the Niagagarega people on several late-17th-century French maps of the area. According to George R. Stewart, it comes from the name of an Iroquois town called Onguiaahra, meaning "point of land cut in two". In 1847, an Iroquois interpreter stated that the name came from Jaonniaka-re, meaning "noisy point or portage". To Mohawks, the name refers to "the neck", pronounced "onyara"; the portage or neck of land between lakes Erie and Ontario onyara.

 

History

Many figures have been suggested as first circulating a European eyewitness description of Niagara Falls. The Frenchman Samuel de Champlain visited the area as early as 1604 during his exploration of what is now Canada, and members of his party reported to him the spectacular waterfalls, which he described in his journals. The first description of the falls is credited to Belgian missionary, Father Louis Hennepin in 1677, after traveling with the explorer René-Robert Cavelier, Sieur de La Salle, thus bringing the falls to the attention of Europeans. French Jesuit missionary Paul Ragueneau likely visited the falls some 35 years before Hennepin's visit while working among the Huron First Nation in Canada. Jean de Brébeuf also may have visited the falls, while spending time with the Neutral Nation. The Finnish-Swedish naturalist Pehr Kalm explored the area in the early 18th century and is credited with the first scientific description of the falls. In 1762, Captain Thomas Davies, a British Army officer and artist, surveyed the area and painted the watercolor, An East View of the Great Cataract of Niagara, the first eyewitness painting of the falls.

 

During the 19th century, tourism became popular, and by the mid-century, it was the area's main industry. Theodosia Burr Alston (daughter of Vice President Aaron Burr) and her husband Joseph Alston were the first recorded couple to honeymoon there in 1801. Napoleon Bonaparte's brother Jérôme visited with his bride in the early 19th century. In 1825, British explorer John Franklin visited the falls while passing through New York en route to Cumberland House as part of his second Arctic expedition, calling them "so justly celebrated as the first in the world for grandeur".

 

In 1843, Frederick Douglass joined the American Anti-Slavery Society's "One Hundred Conventions" tour throughout New York and the midwest. Sometime on this tour, Douglass visited Niagara Falls and wrote a brief account of the experience: "When I came into its awful presence the power of discription failed me, an irrisistible power closed my lips." Being on the Canadian border, Niagara Falls was on one of the routes of the Underground Railroad. The falls were also a popular tourist attraction for Southern slaveowners, who would bring their enslaved workers on the trip. "Many a time the trusted body-servant, or slave-girl, would leave master or mistress in the discharge of some errand, and never come back." This sometimes led to conflict. Early town father Peter Porter assisted slavecatchers in finding runaway slaves, even leading, in the case of runaway Solomon Moseby, to a riot in Niagara-on-the-Lake, Canada. Much of this history is memorialized in the Niagara Falls Underground Railroad Heritage Center. After the American Civil War, the New York Central Railroad publicized Niagara Falls as a focus of pleasure and honeymoon visits. After World War II, the auto industry, along with local tourism boards, began to promote Niagara honeymoons.

 

In about 1840, the English industrial chemist Hugh Lee Pattinson traveled to Canada, stopping at Niagara Falls long enough to make the earliest known photograph of the falls, a daguerreotype in the collection of Newcastle University. It was once believed that the small figure standing silhouetted with a top hat was added by an engraver working from imagination as well as the daguerreotype as his source, but the figure is clearly present in the photograph. Because of the very long exposure required, of ten minutes or more, the figure is assumed by Canada's Niagara Parks agency to be Pattinson. The image is left-right inverted and taken from the Canadian side. Pattinson made other photographs of Horseshoe Falls; these were then transferred to engravings to illustrate Noël Marie Paymal Lerebours' Excursions Daguerriennes (Paris, 1841–1864).[55]

 

On August 6, 1918, an iron scow became stuck on the rocks above the falls. The two men on the scow were rescued, but the vessel remained trapped on rocks in the river, and is still visible there in a deteriorated state, although its position shifted by 50 meters (160 ft) during a storm on October 31, 2019. Daredevil William "Red" Hill Sr. was particularly praised for his role in the rescue.

 

After the First World War, tourism boomed as automobiles made getting to the falls much easier. The story of Niagara Falls in the 20th century is largely that of efforts to harness the energy of the falls for hydroelectric power, and to control the development on both sides that threaten the area's natural beauty. Before the late 20th century, the northeastern end of Horseshoe Falls was in the United States, flowing around the Terrapin Rocks, which were once connected to Goat Island by a series of bridges. In 1955, the area between the rocks and Goat Island was filled in, creating Terrapin Point. In the early 1980s, the U.S. Army Corps of Engineers filled in more land and built diversion dams and retaining walls to force the water away from Terrapin Point. Altogether, 400 ft (120 m) of Horseshoe Falls were eliminated, including 100 ft (30 m) on the Canadian side. According to author Ginger Strand, the Horseshoe Falls is now entirely in Canada. Other sources say "most of" Horseshoe Falls is in Canada.

 

The only recorded freeze-up of the river and falls was caused by an ice jam on March 29, 1848. No water (or at best a trickle) fell for as much as 40 hours. Waterwheels stopped, and mills and factories shut down for having no power. In 1912, American Falls was completely frozen, but the other two falls kept flowing. Although the falls commonly ice up most winters, the river and the falls do not freeze completely. The years 1885, 1902, 1906, 1911, 1932, 1936, 2014, 2017 and 2019 are noted for partial freezing of the falls. A so-called ice bridge was common in certain years at the base of the falls and was used by people who wanted to cross the river before bridges had been built. During some winters, the ice sheet was as thick as 40 to 100 feet (12 to 30 m), but that thickness has not occurred since 1954. The ice bridge of 1841 was said to be at least 100 feet thick. On February 12, 1912, the ice bridge which had formed on January 15 began breaking up while people were still on it. Many escaped, but three died during the event, later named the Ice Bridge Tragedy.

 

Bridge crossings

A number of bridges have spanned the Niagara River in the general vicinity of the falls. The first, not far from the whirlpool, was a suspension bridge above the gorge. It opened for use by the public in July 1848 and remained in use until 1855. A second bridge in the Upper Falls area was commissioned, with two levels or decks, one for use by the Great Western Railway. This Niagara Falls Suspension Bridge opened in 1855. It was used by conductors on the Underground Railroad to escort runaway slaves to Canada. In 1882, the Grand Trunk Railway took over control of the second deck after it absorbed the Great Western company. Significant structural improvements were made in the late 1870s and then in 1886; this bridge remained in use until 1897.

 

Because of the volume of traffic, the decision was made to construct a new arch bridge nearby, under and around the existing bridge. After it opened in September 1897, a decision was made to remove and scrap the railway suspension bridge. This new bridge was initially known as the Niagara Railway Arch, or Lower Steel Arch Bridge; it had two decks, the lower one used for carriages and the upper for trains. In 1937, it was renamed the Whirlpool Rapids Bridge and remains in use today. All of the structures built up to that time were referred to as Lower Niagara bridges and were some distance from the falls.

 

The first bridge in the so-called Upper Niagara area (closer to the falls) was a two-level suspension structure that opened in January 1869; it was destroyed during a severe storm in January 1889. The replacement was built quickly and opened in May 1889. In order to handle heavy traffic, a second bridge was commissioned, slightly closer to American Falls. This one was a steel bridge and opened to traffic in June 1897; it was known as the Upper Steel Arch Bridge but was often called the Honeymoon Bridge. The single level included a track for trolleys and space for carriages and pedestrians. The design led to the bridge being very close to the surface of the river and in January 1938, an ice jam twisted the steel frame of the bridge which later collapsed on January 27, 1938.

 

Another Lower Niagara bridge had been commissioned in 1883 by Cornelius Vanderbilt for use by railways at a location roughly approximately 200 feet south of the Railway Suspension Bridge. This one was of an entirely different design; it was a cantilever bridge to provide greater strength. The Niagara Cantilever Bridge had two cantilevers which were joined by steel sections; it opened officially in December 1883, and improvements were made over the years for a stronger structure. As rail traffic was increasing, the Michigan Central Railroad company decided to build a new bridge in 1923, to be located between the Lower Steel Arch Bridge and the Cantilever Bridge. The Michigan Central Railway Bridge opened in February 1925 and remained in use until the early 21st century. The Cantilever Bridge was removed and scrapped after the new rail bridge opened. Nonetheless, it was inducted into the North America Railway Hall of Fame in 2006.

 

There was a lengthy dispute as to which agency should build the replacement for the Niagara Railway Arch, or Lower Steel Arch Bridge in the Upper Niagara area. When that was resolved, construction of a steel bridge commenced in February 1940. Named the Rainbow Bridge, and featuring two lanes for traffic separated by a barrier, it opened in November 1941 and remains in use today.

 

Industry and commerce

The enormous energy of Niagara Falls has long been recognized as a potential source of power. The first known effort to harness the waters was in 1750, when Daniel Joncaire built a small canal above the falls to power his sawmill. Augustus and Peter Porter purchased this area and all of American Falls in 1805 from the New York state government, and enlarged the original canal to provide hydraulic power for their gristmill and tannery. In 1853, the Niagara Falls Hydraulic Power and Mining Company was chartered, which eventually constructed the canals that would be used to generate electricity. In 1881, under the leadership of Jacob F. Schoellkopf, the Niagara River's first hydroelectric generating station was built. The water fell 86 feet (26 m) and generated direct current electricity, which ran the machinery of local mills and lit up some of the village streets.

 

The Niagara Falls Power Company, a descendant of Schoellkopf's firm, formed the Cataract Company headed by Edward Dean Adams, with the intent of expanding Niagara Falls' power capacity. In 1890, a five-member International Niagara Commission headed by Sir William Thomson among other distinguished scientists deliberated on the expansion of Niagara hydroelectric capacity based on seventeen proposals but could not select any as the best combined project for hydraulic development and distribution. In 1893, Westinghouse Electric (which had built the smaller-scale Ames Hydroelectric Generating Plant near Ophir, Colorado, two years earlier) was hired to design a system to generate alternating current on Niagara Falls, and three years after that a large-scale AC power system was created (activated on August 26, 1895). The Adams Power Plant Transformer House remains as a landmark of the original system.

 

By 1896, financing from moguls including J. P. Morgan, John Jacob Astor IV, and the Vanderbilts had fueled the construction of giant underground conduits leading to turbines generating upwards of 100,000 horsepower (75 MW), sent as far as Buffalo, 20 mi (32 km) away. Some of the original designs for the power transmission plants were created by the Swiss firm Faesch & Piccard, which also constructed the original 5,000 hp (3.7 MW) waterwheels. Private companies on the Canadian side also began to harness the energy of the falls. The Government of Ontario eventually brought power transmission operations under public control in 1906, distributing Niagara's energy to various parts of the Canadian province.

 

Other hydropower plants were being built along the Niagara River. But in 1956, disaster struck when the region's largest hydropower station was partially destroyed in a landslide. This drastically reduced power production and put tens of thousands of manufacturing jobs at stake. In 1957, Congress passed the Niagara Redevelopment Act, which granted the New York Power Authority the right to fully develop the United States' share of the Niagara River's hydroelectric potential.

 

In 1961, when the Niagara Falls hydroelectric project went online, it was the largest hydropower facility in the Western world. Today, Niagara is still the largest electricity producer in New York state, with a generating capacity of 2.4 GW. Up to 1,420 cubic metres (380,000 US gal) of water per second is diverted from the Niagara River through conduits under the city of Niagara Falls to the Lewiston and Robert Moses power plants. Currently between 50% and 75% of the Niagara River's flow is diverted via four huge tunnels that arise far upstream from the waterfalls. The water then passes through hydroelectric turbines that supply power to nearby areas of Canada and the United States before returning to the river well past the falls. When electrical demand is low, the Lewiston units can operate as pumps to transport water from the lower bay back up to the plant's reservoir, allowing this water to be used again during the daytime when electricity use peaks. During peak electrical demand, the same Lewiston pumps are reversed and become generators.

 

To preserve Niagara Falls' natural beauty, a 1950 treaty signed by the U.S. and Canada limited water usage by the power plants. The treaty allows higher summertime diversion at night when tourists are fewer and during the winter months when there are even fewer tourists. This treaty, designed to ensure an "unbroken curtain of water" flowing over the falls, states that during daylight time during the tourist season (April 1 to October 31) there must be 100,000 cubic feet per second (2,800 m3/s) of water flowing over the falls, and during the night and off-tourist season there must be 50,000 cubic feet per second (1,400 m3/s) of water flowing over the falls. This treaty is monitored by the International Niagara Board of Control, using a NOAA gauging station above the falls. During winter, the Power Authority of New York works with Ontario Power Generation to prevent ice on the Niagara River from interfering with power production or causing flooding of shoreline property. One of their joint efforts is an 8,800-foot-long (2,700 m) ice boom, which prevents the buildup of ice, yet allows water to continue flowing downstream. In addition to minimum water volume, the crest of Horseshoe falls was reduced to maintain an uninterrupted "curtain of water".

 

In August 2005, Ontario Power Generation, which is responsible for the Sir Adam Beck stations, started a major civil engineering project, called the Niagara Tunnel Project, to increase power production by building a new 12.7-metre (42 ft) diameter, 10.2-kilometre-long (6.3 mi) water diversion tunnel. It was officially placed into service in March 2013, helping to increase the generating complex's nameplate capacity by 150 megawatts. It did so by tapping water from farther up the Niagara River than was possible with the preexisting arrangement. The tunnel provided new hydroelectricity for approximately 160,000 homes.

 

Transport

Ships can bypass Niagara Falls by means of the Welland Canal, which was improved and incorporated into the Saint Lawrence Seaway in the mid-1950s. While the seaway diverted water traffic from nearby Buffalo and led to the demise of its steel and grain mills, other industries in the Niagara River valley flourished with the help of the electric power produced by the river. However, since the 1970s the region has declined economically.

 

The cities of Niagara Falls, Ontario, Canada, and Niagara Falls, New York, United States, are connected by two international bridges. The Rainbow Bridge, just downriver from the falls, affords the closest view of the falls and is open to non-commercial vehicle traffic and pedestrians. The Whirlpool Rapids Bridge lies one mile (1.6 km) north of the Rainbow Bridge and is the oldest bridge over the Niagara River. Nearby Niagara Falls International Airport and Buffalo Niagara International Airport were named after the waterfall, as were Niagara University, countless local businesses, and even an asteroid.

 

Over the falls

The first recorded publicity stunt using the Falls was the wreck of the schooner Michigan in 1827. Local hotel owners acquired a former Lake Erie freighter, loaded it with animals and effigies of people, towed it to a spot above the falls and let it plunge over the brink. Admission of fifty cents was charged.

 

In October 1829, Sam Patch, who called himself "the Yankee Leapster", jumped from a high tower into the gorge below the falls and survived; this began a long tradition of daredevils trying to go over the falls. Englishman Captain Matthew Webb, the first man to swim the English Channel, drowned in 1883 trying to swim the rapids downriver from the falls.

 

On October 24, 1901, 63-year-old Michigan school teacher Annie Edson Taylor became the first person to go over the falls in a barrel as a publicity stunt; she survived, bleeding, but otherwise unharmed. Soon after exiting the barrel, she said, "No one ought ever do that again." Days before Taylor's attempt, her domestic cat was sent over the falls in her barrel to test its strength. The cat survived the plunge unharmed and later posed with Taylor in photographs. Since Taylor's historic ride, over a dozen people have intentionally gone over the falls in or on a device, despite her advice. Some have survived unharmed, but others have drowned or been severely injured. Survivors face charges and stiff fines, as it is now illegal, on both sides of the border, to attempt to go over the falls. Charles Stephens, a 58-year-old barber from Bristol, England, went over the falls in a wooden barrel in July 1920 and was the first person to die in an endeavor of this type. Bobby Leach went over Horseshoe Falls in a crude steel barrel in 1911 and needed rescuing by William "Red" Hill Sr. Hill again came to the rescue of Leach following his failed attempt to swim the Niagara Gorge in 1920. In 1928, "Smiling Jean" Lussier tried an entirely different concept, going over the falls in a large rubber ball; he was successful and survived the ordeal.

  

Annie Edson Taylor posing with her wooden barrel (1901)

In the "Miracle at Niagara", on July 9, 1960, Roger Woodward, a seven-year-old American boy, was swept over Horseshoe Falls after the boat in which he was cruising lost power; two tourists pulled his 17-year-old sister Deanne from the river only 20 ft (6.1 m) from the lip of the Horseshoe Falls at Goat Island. Minutes later, Woodward was plucked from the roiling plunge pool beneath Horseshoe Falls after grabbing a life ring thrown to him by the crew of the Maid of the Mist boat. The children's uncle, Jim Honeycutt, who had been steering the boat, was swept over the edge to his death.

 

On July 2, 1984, Canadian Karel Soucek from Hamilton, Ontario, plunged over Horseshoe Falls in a barrel with only minor injuries. Soucek was fined $500 for performing the stunt without a license. In 1985, he was fatally injured while attempting to re-create the Niagara drop at the Houston Astrodome. His aim was to climb into a barrel hoisted to the rafters of the Astrodome and to drop 180 ft (55 m) into a water tank on the floor. After his barrel released prematurely, it hit the side of the tank, and he died the next day from his injuries.

 

In August 1985, Steve Trotter, an aspiring stuntman from Rhode Island, became the youngest person ever (age 22) and the first American in 25 years to go over the falls in a barrel. Ten years later, Trotter went over the falls again, becoming the second person to go over the falls twice and survive. It was also the second "duo"; Lori Martin joined Trotter for the barrel ride over the falls. They survived the fall, but their barrel became stuck at the bottom of the falls, requiring a rescue.

 

On September 28, 1989, Niagara natives Peter DeBernardi and Jeffery James Petkovich became the first "team" to make it over the falls in a two-person barrel. The stunt was conceived by DeBenardi, who wanted to discourage youth from following in his path of addictive drug use. The pair emerged shortly after going over with minor injuries and were charged with performing an illegal stunt under the Niagara Parks Act.

 

On June 5, 1990, Jesse Sharp, a whitewater canoeist from Tennessee paddled over the falls in a closed deck canoe. He chose not to wear a helmet to make his face more visible for photographs of the event. He also did not wear a life vest because he believed it would hinder his escape from the hydraulics at the base of the falls. His boat flushed out of the falls, but his body was never found. On September 27, 1993, John "David" Munday, of Caistor Centre, Ontario, completed his second journey over the falls. On October 1, 1995, Robert Douglas "Firecracker" Overacker went over the falls on a Jet Ski to raise awareness for the homeless. His rocket-propelled parachute failed to open and he plunged to his death. Overacker's body was recovered before he was pronounced dead at Niagara General Hospital.

 

Kirk Jones of Canton, Michigan, became the first known person to survive a plunge over Horseshoe Falls without a flotation device on October 20, 2003. According to some reports, Jones had attempted to commit suicide, but he survived the fall with only battered ribs, scrapes, and bruises. Jones tried going over the falls again in 2017, using a large inflatable ball, but died in the process. Later reports revealed that Jones had arranged for a friend to shoot video clips of his stunt.

 

On March 11, 2009, a man survived an unprotected trip over Horseshoe Falls. When rescued from the river he suffered from severe hypothermia and a large wound to his head. His identity was never released. Eyewitnesses reported seeing the man intentionally enter the water. On May 21, 2012, an unidentified man became the fourth person to survive an unprotected trip over Horseshoe Falls. Eyewitness reports show he "deliberately jumped" into the Niagara River after climbing over a railing. On July 8, 2019, at roughly 4 am, officers responded to a report of a person in crisis at the brink of the Canadian side of the falls. Once officers got to the scene, the man climbed the retaining wall, jumped into the river and went over Horseshoe Falls. Authorities subsequently began to search the lower Niagara River basin, where the man was found alive but injured sitting on the rocks at the water's edge.

 

Tightrope walkers

Tightrope walkers drew huge crowds to witness their exploits. Their wires ran across the gorge, near the current Rainbow Bridge, not over the waterfall. Jean François "Blondin" Gravelet was the first to cross Niagara Gorge on June 30, 1859, and did so again eight times that year. His most difficult crossing occurred on August 14, when he carried his manager, Harry Colcord, on his back.[114] His final crossing, on September 8, 1860, was witnessed by the Prince of Wales. Author Ginger Strand argues that these performances may have had symbolic meanings at the time relating to slavery and abolition.

 

Between 1859 and 1896 a wire-walking craze emerged, resulting in frequent feats over the river below the falls. One inexperienced walker slid down his safety rope. Only one man fell to his death, at night and under mysterious circumstances, at the anchoring place for his wire.

 

Maria Spelterini, a 23-year-old Italian was the first and only woman to cross the Niagara River gorge; she did so on a tightrope on July 8, 1876. She repeated the stunt several times during the same month. During one crossing she was blindfolded and during another, her ankles and wrists were handcuffed.

 

Among the many competitors was Ontario's William Hunt, who billed himself as "The Great Farini"; his first crossing was in 1860. Farini competed with Blondin in performing outrageous stunts over the gorge. On August 8, 1864, however, an attempt failed and he needed to be rescued.

 

On June 15, 2012, high wire artist Nik Wallenda became the first person to walk across the falls area in 116 years, after receiving special permission from both governments. The full length of his tightrope was 1,800 feet (550 m). Wallenda crossed near the brink of Horseshoe Falls, unlike walkers who had crossed farther downstream. According to Wallenda, it was the longest unsupported tightrope walk in history. He carried his passport on the trip and was required to present it upon arrival on the Canadian side of the falls.

 

Tourism

A ring-billed gull flies by a rainbow over the Horseshoe Falls

Peak visitor traffic occurs in the summertime, when Niagara Falls is both a daytime and evening attraction. From the Canadian side, floodlights illuminate both sides of the falls for several hours after dark (until midnight). The number of visitors in 2007 was expected to total 20 million, and by 2009 the annual rate was expected to top 28 million tourists.

 

The oldest and best known tourist attraction at Niagara Falls is the Maid of the Mist boat cruise, named for an alleged ancient Ongiara Indian mythical character, which has carried passengers into the rapids immediately below the falls since 1846. Cruise boats operate from boat docks on both sides of the falls, with the Maid of the Mist operating from the American side and Hornblower Cruises (originally Maid of the Mist until 2014) from the Canadian side. In 1996, Native American groups threatened to boycott the boat companies if they would not stop playing what they said was a fake story on their boats. The Maid of the Mist dropped the audio.

 

From the U.S. side, American Falls can be viewed from walkways along Prospect Point Park, which also features the Prospect Point Observation Tower and a boat dock for the Maid of the Mist. Goat Island offers more views of the falls and is accessible by foot and automobile traffic by bridge above American Falls. From Goat Island, the Cave of the Winds is accessible by elevator and leads hikers to a point beneath Bridal Veil Falls. Also on Goat Island are the Three Sisters Islands, the Power Portal where a statue of Nikola Tesla (the inventor whose patents for the AC induction motor and other devices for AC power transmission helped make the harnessing of the falls possible) can be seen, and a walking path that enables views of the rapids, the Niagara River, the gorge, and all of the falls. Most of these attractions lie within the Niagara Falls State Park.

 

The Niagara Scenic Trolley offers guided trips along American Falls and around Goat Island. Panoramic and aerial views of the falls can also be viewed by helicopter. The Niagara Gorge Discovery Center showcases the natural and local history of Niagara Falls and the Niagara Gorge. A casino and luxury hotel was opened in Niagara Falls, New York, by the Seneca Indian tribe. The Seneca Niagara Casino & Hotel occupies the former Niagara Falls Convention Center. The new hotel is the first addition to the city's skyline since completion of the United Office Building in the 1920s.

 

On the Canadian side, Queen Victoria Park features manicured gardens, platforms offering views of American, Bridal Veil, and Horseshoe Falls, and underground walkways leading into observation rooms that yield the illusion of being within the falling waters. Along the Niagara River, the Niagara River Recreational Trail runs 35 mi (56 km) from Fort Erie to Fort George, and includes many historical sites from the War of 1812.

 

The observation deck of the nearby Skylon Tower offers the highest view of the falls, and in the opposite direction gives views as far as Toronto. Along with the Tower Hotel (built as the Seagrams Tower, later renamed the Heritage Tower, the Royal Inn Tower, the Royal Center Tower, the Panasonic Tower, the Minolta Tower, and most recently the Konica Minolta Tower before receiving its current name in 2010), it is one of two towers in Canada with a view of the falls. The Whirlpool Aero Car, built in 1916 from a design by Spanish engineer Leonardo Torres Quevedo, is a cable car that takes passengers over the Niagara Whirlpool on the Canadian side. The Journey Behind the Falls consists of an observation platform and series of tunnels near the bottom of the Horseshoe Falls on the Canadian side. There are two casinos on the Canadian side of Niagara Falls, the Niagara Fallsview Casino Resort and Casino Niagara.

 

Touring by helicopter over the falls, from both the US and the Canadian side, was described by The New York Times as still popular a year after a serious crash. Although The New York Times had long before described attempting to tour the falls as "bent on suicide" and despite a number of fatal crashes, the "as many as 100 eight-minute rides each day" are hard to regulate; two countries and various government agencies would have to coordinate. These flights have been available "since the early 1960s."

Average result given I don't like movements up against platforms. I had gone to Upper Holloway as the 1Q97 Ferme Park to Cambridge test train with 37219 and 37175 was due to run into the bi directional goods loop here, but it went off route and straight to East London via an alternative route. 59002 works a Purfleet to Action TC yard of empty boxes on Wednesday 24 June 2020

2011-Cmeo(Cemo),Dasr,Rosek(Neist),Urge,Aseb,Revert

 

Ec-Bsf-Rarekind-Mct-Gf-Chm-Greetings- Pm

 

original size photo(click it):

images.imagehotel.net/?q2lv5md2fb.jpg#null

Only a minute and a half (as permitted by flickr) of fairly average video, but one which aught to be of some interest to our Portuguese friends and indeed anyone who enjoys scenic narrow gauge railways.

The Metre gauge Tua Valley line was the most easterly of the three surviving narrow gauge tributaries to the main Douro Valley line which just about made it into the 21st century. In recent times it ran from it's interchange through some initially spectacular scenery to a truncated terminus at Mirandela.

As local roads improved with the aid of EU cash at a similar time to CP (Portuguese Railways) feeling the financial pinch, the line ... and indeed all three, were unceremoniously closed.

This little video piece was recorded in the late 1990s when the meagre service was loco hauled using two or three coaches and a 1000hp Alsthom built Bo-Bo Diesel Electric. In the last days, it became the province of a single railcar.

Such was the carefree attitude which prevailed in Portugal at the time, I was able to film away from the open vestibule door whilst my travelling companion held onto my collar! I'd expected we might be in bother when it came time for a ticket check, but a quick glance from the guard at ours and away he went leaving us to do as we pleased. The line and particularly the trip up this spectacular gorge is much lamented ... Such a potential tourist draw in 90% of other EU countries would have ensured the operation would have had a secure future in that sector, but sadly, not in Portugal.

Average seeing conditions. Photographed from Northwich, UK at 00:00 UT. 6000 1/110s colour exposures stacked. Player One Uranus-C / 12" Meade LX200 at f/23.5.

This and all South Telegraph designs are its sole property and cannot be resold or republished.

Goal: To create a branding package for an upcoming series titled chosen.

Audience: Adult weekend service.

Direction: The pastor told me this series was going to be on the life of Joseph...and all he had was the title "Not Your Average Joe" He didn't really have any direction for me and just asked me to throw some concepts at him. This is the one he went with. I decided to used the way we customize the perfect "cup of Joe" as a metaphor for how the key ingredients were present in Joseph's life to make him a great man of God. The boxes on the front of the coffee cup will be the topic for each week's sermon.

Project: Freelance project: Clockwise from top left: Bulletin outside, Bulletin inside, Home page rotator, Sermon web banner, Postcard mailer, Power point for notes, Power point opener.

Colour / Silver Efex average.

Buffy Fish Owl (Ketupa ketupu)

 

The buffy fish owl (Bubo ketupu), also known as the Malay fish owl, is a species of owl in the Strigidae family.

 

The four fish owls were previously generally separated in the genus Ketupa. mtDNA cytochrome b sequence data is equivocal on which genus name is applied for them, and today they are commonly lumped with the horned and eagle-owls (Bubo) – which they also resemble osteologically very much – for sake of convenience. Depending on whether some little-studied tropical eagle-owls are closer to the fish-owls than to the typical eagle-owls, Ketupa might be a valid genus if these as well as the fishing owls (formerly Scotopelia) are included in it, although there are a number of osteological differences that suggest that fishing and fish owls are not directly related to each other.

  

Distribution and habitat

 

It is found from southern Burma and central India to the south and east to Cambodia, Laos and Vietnam, peninsular Thailand, the Malay Peninsula, the Riau Archipelago, Sumatra Brunei, Cocos (Keeling) Islands, Indonesia down to Java, Bali and Borneo. One specimen was recorded at Cocos (Keeling) Island off Australia, 1,050 km (650 mi) outside its regular range. Its natural habitat is wet tropical forests and other woody areas near water, including wooded banks of rivers, lakes and fish ponds and rich paddies. It can survive well close to human habitations but can also be found in desolate mangrove forests and other less-inhabited or uninhabited areas. It mainly lives in lowlands but can be found at up an elevation of 1,600 m (5,200 ft).

  

Description

 

The buffy fish owl is a fairly large owl but is the smallest of the four species of fish owl. In total length, this species can range from 38 to 48 cm (15 to 19 in). Body mass can range from 1,028 to 2,100 g (2.266 to 4.630 lb), with an average weight of 1,224 g (2.698 lb). This species is yellowish-brown overall, with considerable variegating with pale buff. The feathers are edged tawny and the wings and tail are broadly barred yellowish and dark brown. The wings are distinctly rounded in shape when this species is seen in flight. The underparts are a yellow-brown, rich buff or fulvous color with broad blackish shaft-stripes. The legs are long and unfeathered. This species slightly overlaps in range with the brown fish owl, but that species is slightly larger and coniserably more brown in overall color with stronger barring and vermiculations below. The tawny fish owl may also marginally overlap with the buffy fish owl in range and is also larger with a much richer tawny color with a more barred tail, a whiter face and about two-thirds of its tarsi feathered. Like all fish owls, the buffy fish owl has prominent ear tufts but they hang to the sides of the head rather than sit atop and are scraggly looking. This species has been attributed with a range of vocalizations. Among these recorded have included hissing sounds and a rattling kutook, repeatedly rapidly about seven times. Also recorded has been a ringing, loud pof-pof-pof and a high, hawk-like hie-e-e-e-e-keek series of notes. The buffy fish owl is rather noisy before breeding and pairs may engage in bouts of duetting for several minutes at a time.

 

Compared to eagle owls of similar length, fish owls tend to be even shorter in tail length and even heavier in build, have relatively larger wings (the tawny and Blakiston's being particularly chunky in shape), have considerably longer legs, and have a rough texture to the bottom of their toes. At least the latter two features are clear adaptations to aid these owls in capturing fish. Diurnal raptors who feed largely on fish have similar, if not identical, rough texture under their toes, which helps these birds grasp slippery fish. Unlike diurnal raptors who capture fish such as the osprey (Pandion haliaetus) as compared to most terrestrial raptors, the fish owls have large, powerful, and curved talons and a longitudinal sharp keel sitting under the middle claw with all having sharp cutting edges that are very much like those of eagle owls. Also, unlike fish-eating diurnal raptors will not submerge any part of their body while hunting, preferring only to put their feet into the water, although fish owls will hunt on foot, wading into the shallows. Unlike most owls, the feathers of fish owls are not soft to the touch and they lack the comb and hair-like fringes to the primaries, which allow other owls to fly silently in order to ambush their prey. Due to the lack of these feather-specializations, fish owl wing beats make sounds. The lack of a deep facial disc in fish owls is another indication of the unimportance of sound relative to vision in these owls, as facial disc depth (as well as inner ear size) are directly related to how important sound is to an owl's hunting behavior. Also different from most any other kind of owl, the bill is placed on the face between the eyes rather below it, which is said to impart this fish owl with a "remarkably morose and sinister expression". Similar adaptations, such as unwillingness to submerge beyond their legs and lack of sound-muffling feathers are also seen in the African fishing owls, which do not seem to be directly related. Due to their neat replacement of each other in range, at one time the tawny and buffy fish owls were considered the same species but there are a number of physical, anatomical, habitat and behavioral distinctions between them.

  

Ecology and behavior

 

During the daytime, these owls shelter, often singly, in quite dark places, such as densely foliaged trees. Buffy fish owls are easily disturbed, quite the opposite of the highly stoic tawny fish owl, often being wide-awake before being spotted by a human observer. The largest part of its diet appears to consist of fish, crabs and frogs followed by reptiles, toads and crayfish. Their diet is not extensively studied but appears to be basically the same as those of the brown and tawny fish owls. Rats, mice and large insects are also sometimes taken and even bats have been captured by this species. A small handful of prey has been identified to genera or species in Java: goldfish (Carassius auratus), the gold-ringed cat snake (Boiga dendrophila), puff-faced water snake (Homalopsis buccata), young false gharials (Tomistoma schlegelii), fruit bats (Cynopterus ssp.), centipedes (Scolopendra ssp.), black rats (Rattus rattus) and red junglefowl (Gallus gallus bankiva), some of this prey such as the cat snake and junglefowl being of a fairly large size. Like the brown fish owl but unlike most owls, this species has been recorded consuming carrion, including the remains of a crocodile and a Sunda stink badger (Mydaus javanensis). The buffy fish owl does not produce firm pellets as do most owls. Instead bones and frog and insect remains are ejected in pieces and fall to the ground below roost. Prey remains have only been found within the nest, never around or below the nest as is commonly recorded in other owls. The buffy fish owl hunts mainly from the bank, swooping down much in the manner of a fish eagle but never getting its feathers wet. It also walks into shawllow streams and brooks, additionally snatching their main foods in such locations.

 

Eggs have mainly been found in February through April, less commonly into May through July, as in western Java, and even in September through January in the Malay Peninsula. The buffy fish owl frequently nest on top of a large fern (Asplenium nidus), but nests have also been recorded in the fork a tall bough covered in ferns and moss, on orchid beds and in tree holes. More rarely, rocky sites have been used as nesting sites, even behind waterfalls. The nest is usually merely a scrap into the surface of a fern with no structure or lining, as owls do not build nests. Abandoned bird nests built by other species have been used, including those of Brahminy kites (Haliastur indus). Only one egg has ever been recorded in a buffy fish owl nest, giving them the smallest clutch size of any owl alongside the spot-bellied eagle owl (B. nipalensis), which has only ever been recorded with a single-egg clutch. The egg is round, oval and dull white. The average dimensions of eggs in western Java was 57.4 mm × 47 mm (2.26 in × 1.85 in). Incubation of the eggs lasts 28-29 days and fledgling occurs after six weeks. This species is generally faring well for a large raptorial bird and has been inadvertently aided by commercial fisheries and ornamental ponds, which they visit by night to hunt. Sometimes, they incure persecution from owners of such ponds for taking stock.

  

[credit: en.wikipedia.org/]

  

Quaint vietnamese restaurant with very average food

Just your average group of 8th grade friends until a there basement hang out collapsed beneath them leaving them in uncharted territory...

 

Jeff, is Jeff he just happens to be really tall. I mean really tall and seems to get taller when needed.

yeah, I know, it's an average shot, but it's the best I could do without a big lens. 'o)

Prairie dogs (Cynomys) are burrowing rodents native to the grasslands of North America. They are a type of ground squirrel. On average, these stout-bodied rodents will grow to be between 30–40 centimetres (12–16 in) long, including the short tail and weigh between 0.5–1.5 kilograms (1–3 lb). They are found in the United States, Canada, and Mexico. In Mexico, prairie dogs are primarily found in the northern states which are the southern end of the great plains: northeastern Sonora, north and northeastern Chihuahua, northern Coahuila, northern Nuevo León, and northern Tamaulipas; in the U.S., they range primarily west of the Mississippi River, though they have also been introduced in a few eastern locales. They will eat all sorts of vegetables and fruits.Prairie dogs raise their heads from their burrows in response to disturbancesPrairie dogs are named for their habitat and warning call, which sounds similar to a dog's bark. Its genus, Cynomys, derives from the Greek for dog mouse.Highly social, prairie dogs live in large colonies or "towns" – collections of prairie dog families that can span hundreds of acres. Families usually consist of 1 male and 2 to 4 females living in a strict social hierarchy. Prairie dog pups reach sexual maturity at about 3 years of age, and after their third winter the dominant male in a given family will drive them away, forcing them to establish their own families on the edges of the colony. The dominant male will defend the family's borders against rival prairie dogs, and disputes are resolved by fighting. Prairie dogs are also aggressive against predators such as badgers and snakes. Prairie dogs are social animals, however, and often make social visits with each other, and greet each other with a sort of kiss.[5] Prairie dogs employ a complex form of communication that involves barks and rhythmic chirps.

Prairie dogs showing affectionPrairie dog tunnel systems help channel rainwater into the water table to prevent runoff and erosion, and can also serve to change the composition of the soil in a region by reversing soil compaction that can be a result of cattle grazing. The tunnels usually have several chambers. Tunnels can descend vertically as much as 5 metres (16 ft), and can extend laterally as much as 30 metres (98 ft). Prairie dogs line their burrows with grass to insulate them, and the earth excavated from the burrow is piled up in mounds around the burrow's entrance. The prairie dogs use these carefully maintained mounds as observation posts.The prairie dog is well adapted to predators. Using its dichromatic color vision, it can detect predators from a far distance and then alert other prairie dogs to the danger with a special, high-pitched call. Con Slobodchikoff and others assert that prairie dogs use a sophisticated system of vocal communication to describe specific predators. Prairie dogs also trim the vegetation around their colonies, perhaps to remove any cover for predators. Their burrows generally contain several routes of escape.The prairie dog is chiefly herbivorous, though it eats some insects. It feeds primarily on grasses and, in the fall, broadleaf forbs. Prairie dogs have 1-6 pups (babies) yearly, which are born blind and furless and need about 30 days of close nurturing from their mother.Sometimes two prairie dogs touch teeth with each other. Researchers think they do this as a way of recognizing each other.

 

I cani della prateria (Cynomys) sono un genere di mammiferi appartenenti all'ordine dei Roditori e alla famiglia Sciuridae, indigeno delle praterie americane.

Nonostante il nome, non sono dunque canidi, bensì roditori, della stessa famiglia delle marmotte. Devono il loro nome ad un suono, simile ad un latrato, che emettono in caso di pericolo. Diversamente dalle marmotte, non vanno in letargo.Pesano da 800 a 1500 gr per ca 30-35 cm di lunghezza.Sono animali estremamente socievoli e vivono in larghe colonie, formate da gruppi familiari di un maschio, 3-4 femmine e i piccoli dell'anno. La femmina, dopo una gestazione di 36 giorni, mette al mondo da 2 a 4 piccoli, che nascono molto immaturi e necessitano delle cure materne prima di poter uscire dal nido per almeno altri 30 giorni. Allo stato selvatico vivono per circa 5 anni, in cattività fino a 8 o 10.I cani della prateria sono animali dotati di elevata intelligenza e capaci di emettere più di 25 suoni diversi in base al tipo di pericolo che si avvicina (un uccello, un bovino, un uomo ecc.).

 

Font : Wikipedia

 

www.parconaturaviva.it/

Ash is a large village, now almost a town, now bypassed by the Canterbury to Sandwich road.

 

St Nicholas is a large church, and sits on a low mound above the High Street and houses.

 

The church itself is cruciform in shape, and previously stated, large.

 

It is furnished with serval monuments and brasses, all of a very high standard.

 

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A large and impressive church of mainly thirteenth century date over restored in 1847 by the irrepressible William Butterfield. The scale of the interior is amazing - particularly in the tower crossing arches which support the enormous spire. They are an obvious insertion into an earlier structure. The best furnishing at Ash is the eighteenth century font which stands on an inscribed base. For the visitor interested in memorials, Ash ahs more than most ranging from the fourteenth century effigy of a knight to two excellent alabaster memorials to Sir Thomas Harfleet (d 1612) and Christopher Toldervy (d 1618). Mrs Toldervy appears twice in the church for she accompanies her husband on his memorial and may also be seen as a `weeper` on her parents` memorial! On that she is one of two survivors of what was once a group of seven daughters - all her weeping brothers have long since disappeared.

 

www.kentchurches.info/church.asp?p=Ash+2

 

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ASH

LIES adjoining to the last-described parish of Staple northward. It is written in Domesday, Ece, and in other antient records, Aisse, and is usually called Ash, near Sandwich, to distinguish it from Ash, near Wrotham.

 

The parish of Ash is very large, extending over a variety of soil and country, of hill, dale, and marsh lands, near four miles across each way, and containing more than six thousand acres of land, of which about one half is marsh, the river Stour being its northern bounday, where it is very wet and unwholesone, but the southern or upland part of the parish is very dary, pleasant and healthy. The soil in general is fertile, and lets on an average at about one pound an acre; notwithstanding, there is a part of it about Ash-street and Gilton town, where it is a deep sand. The village of Ash, commonly called Ash-street, situated in this part of it, on high ground, mostly on the western declivity of a hill, having the church on the brow of it, is built on each side of the road from Canterbury to Sandwich, and contains about fifty houses. On the south side of this road, about half a mile westward, is a Roman burial ground, of which further mention will be taken hereaster, and adjoining to it the hamlet of Gilton town, formerly written Guildanton, in which is Gilton parsonage, a neat stuccoed house, lately inhabited by Mr. Robert Legrand, and now by Mrs. Becker. In the valley southward stands Mote farm, alias Brooke house, formerly the habitation of the Stoughtons, then of the Ptoroude's and now the property of Edward Solly, esq. of London.

 

There are dispersed throughout this large parish many small hamlets and farms, which have been formerly of more consequence, from the respective owners and in habitants of them, all which, excepting East and New Street, and Great Pedding, (the latter of which was the antient residence of the family of solly, who lie buried in Ash church-yard, and bore for their arms, Vert, a chevron, per pale, or, and gules, between three soles naiant, argent, and being sold by one of them to dean Lynch, is now in the possession of lady Lynch, the widow of Sir William Lynch, K. B.) are situated in the northern part of the parish, and contain together about two hundred and fifty houses, among them is Hoden, formerly the residence of the family of St. Nicholas; Paramour-street, which for many years was the residence of those of that name, and Brook-street, in which is Brook-house, the residence of the Brooke's, one of whom John Brooke, esq. in queen Elizabeth's reign, resided here, and bore for his arms, Per bend, vert and sable, two eagles, counterchanged.

 

William, lord Latimer, anno 38 Edward III. obtained a market to be held at Ash, on a Thursday; and a fair yearly on Lady-day, and the two following ones. A fair is now held in Ash-street on Lady and Michaelmas days yearly.

 

In 1473 there was a lazar house for the infirm of the leprosy, at Eche, near Sandwich.

 

¶The manor of Wingham claims paramount over this parish, subordinate to which there were several manors in it, held of the archbishop, to whom that manor belonged, the mansions of which, being inhabited by families of reputation and of good rank in life, made this parish of much greater account than it has been for many years past, the mansions of them having been converted for a length of time into farmhouses to the lands to which they belong.

 

f this manor, (viz. Wingham) William de Acris holds one suling in Fletes, and there he has in demesne one carucate and four villeins, and one knight with one carucate, and one fisbery, with a saltpit of thirty pence. The whole is worth forty shillings.

 

This district or manor was granted by archbishop Lanfranc, soon after this, to one Osberne, (fn. 7) of whom I find no further mention, nor of this place, till king Henry III.'s reign, when it seems to have been separated into two manors, one of which, now known by the name of the manor of Gurson Fleet, though till of late time by that of Fleet only, was held afterwards of the archbishop by knight's service, by the family of Sandwich, and afterwards by the Veres, earls of Oxford, one of whom, Robert de Vere, earl of Oxford, who died anno 3 Edward III. was found by the escheat-rolls of that year, to have died possessed of this manor of Fleet, which continued in his descendants down to John de Vere, earl of Oxford, who for his attachment to the house of Lancaster, was attainted in the first year of king Edward IV. upon which this manor came into the hands of the crown, and was granted the next year to Richard, duke of Gloucester, the king's brother, with whom it staid after his succession to the crown, as king Richard III. on whose death, and the accession of king Henry VII. this manor returned to the possession of John, earl of Oxford, who had been attainted, but was by parliament anno I Henry VII. restored in blood, titles and possessions. After which this manor continued in his name and family till about the middle of queen Elizabeth's reign, when Edward Vere, earl of Oxford, alienated it to Hammond, in whose descendants it continued till one of them, in the middle of king Charles II.'s reign, sold it to Thomas Turner, D. D. who died possessed of it in 1672, and in his name and descendants it continued till the year 1748, when it was sold to John Lynch, D. D. dean of Canterbury, whose son Sir William Lynch, K. B. died possessed of it in 1785, and by his will devised it, with the rest of his estates, to his widow lady Lynch, who is the present possessor of it. A court baron is held for this manor.

 

Archbishop Lanfranc, on his founding the priory of St. Gregory, in the reign of the Conqueror, gave to it the tithe of the manor of Fleet; which gift was confirmed by archbishop Hubert in Richard I.'s reign. This portion of tithes, which arose principally from Gurson Fleet manor, remained with the priory at its dissolution, and is now part of Goldston parsonage, parcel of the see of Canterbury, of which further mention has been made before.

 

The other part of the district of Fleet was called, to distinguish it, and from the possessors of it, the manor of Nevills Fleet, though now known by the name of Fleet only, is situated between Gurson and Richborough, adjoining to the former. This manor was held in king John's reign of the archbishop, by knight's service, by Thomas Pincerna, so called probably from his office of chief butler to that prince, whence his successors assumed the name of Butler, or Boteler. His descendant was Robert le Boteler, who possessed this manor in king Ed ward I.'s reign, and from their possession of it, this manor acquired for some time the name of Butlers Fleet; but in the 20th year of king Edward III. William, lord Latimer of Corbie, appears to have been in the possession of it, and from him it acquired the name of Latimers Fleet. He bore for his arms, Gules, a cross flory, or. After having had summons to parliament, (fn. 8) he died in the begening of king Richard II.'s reign, leaving Elizabeth his sole daughter and heir, married to John, lord Nevill, of Raby, whose son John bore the title of lord Latimer, and was summoned to parliament as lord Latimer, till the 9th year of king Henry VI. in which he died, so that the greatest part of his inheritance, among which was this manor, came by an entail made, to Ralph, lord Nevill, and first earl of Westmoreland, his eldest, but half brother, to whom he had sold, after his life, the barony of Latimer, and he, by seoffment, vested it, with this manor and much of the inheritance above-mentioned, in his younger son Sir George Nevill, who was accordingly summoned to parliament as lord Latimer, anno 10 Henry VI. and his grandson Richard, lord Latimer, in the next regin of Edward IV. alienated this manor, which from their length of possession of it, had acquired the name of Nevill's Fleet, to Sir James Cromer, and his son Sir William Cromer, in the 11th year of king Henry VII, sold it to John Isaak, who passed it away to Kendall, and he, in the beginning of king Henry VIII.'s reign, sold it to Sir John Fogge, of Repton, in Ashford, who died possessed of it in 1533, and his son, of the same name, before the end of it, passed it away to Mr. Thomas Rolfe, and he sold it, within a few years afterwards, to Stephen Hougham, gent. of this parish, who by his will in 1555, devised it to his youngest son Rich. Hougham, of Eastry, from one of whose descendants it was alienated to Sir Adam Spracklin, who sold it to one of the family of Septvans, alias Harflete, in which name it continued till within a few years after the death of king Charles I. when by a female heir Elizabeth it went in marriage to Thomas Kitchell, esq. in whose heirs it continued till it was at length, about the year 1720, alienated by one of them to Mr. Thomas Bambridge, warden of the Fleet prison, upon whose death it became vested in his heirs-at-law, Mr. James Bambridge, of the Temple, attorney at-law, and Thomas Bambridge, and they divided this estate, and that part of it allotted to the latter was soon afterwards alienated by him to Mr. Peter Moulson, of London, whose only daughter and heir carried it in marriage to Mr. Geo. Vaughan, of London, and he and the assignees of Mr. James Bambridge last mentioned, have lately joined in the conveyance of the whole fee of this manor to Mr. Joseph Solly, gent. of Sandwich, the present owner of it. There is not any court held for this manor.

 

In this district, and within this manor of Fleet lastmentioned, there was formerly a chapel of cose to the church of Ash, as that was to the church of Wingham, to which college, on its foundation by archbishop Peckham in 1286, the tithes, rents, obventions, &c of this chapel and district was granted by him, for the support in common of the provost and canons of it, with whom it remained till the suppression of it, anno I king Edward VI. The tithes, arising from this manor of Fleet, and the hamlet of Richborough, are now a part of the rectory of Ash, and of that particular part of it called Gilton parsonage, parcel of the possessions of the see of Canterbury, of which further mention will be made hereafter. There have not been any remains left of it for a long time part.

 

Richborough is a hamlet and district of land, in the south-east part of this parish, rendered famous from the Roman fort and town built there, and more so formerly, from the port or haven close adjoining to it.

 

It was in general called by the Romans by the plural name of Rutupiæ; for it must be observed that the æstuary, which at that time separated the Isle of Thanet from the main land of Kent, and was the general passage for shipping,had at each mouth of it, towards the sea, a fort and haven, called jointly Rutupiæ. That at the northern part and of it being now called Reculver, and that at the eastern, being the principal one, this of Richborough.

 

The name of it is variously spelt in different authors. By Ptolemy it is written [Patapiaia (?)] urbem; by Tacitus, according to the best reading, Portus, Rutupensis; by Antonine, in his Itinerary, Ritupas, and Ritupis Portum; by Ammianus, Ritupiæ statio; afterwards by the Saxons, Reptacester, and now Richborough.

 

The haven, or Portus Rutupinus, or Richborough, was very eminent in the time of the Romans, and much celebrated in antient history, being a safe and commodious harbour, stationem ex adverso tranquillam, as Ammianus calls it, situated at the entrance of the passage towards then Thamas, and becoming the general place of setting sail from Britain to the continent, and where the Roman fleets arrived, and so large and extensive was the bay of it, that it is supposed to have extended far beyond Sandwich on the one side, almost to Ramsgate cliffs on the other, near five miles in width, covering the whole of that flat of land on which Stonar and Sandwich were afterwards built, and extending from thence up the æstuary between the Isle of Thanet and the main land. So that Antonine might well name it the Port, in his Itinerary, [Kat exochin], from there being no other of like consequence, and from this circumstance the shore for some distance on each side acquired the general name of Littus Rutupinum, the Rutupian shore. (fn. 9) Some have contended that Julius Cæsar landed at Richborough, in his expeditions into Britain; but this opinion is refuted by Dr. Hasley in Phil, Trans. No. 193, who plainly proves his place of landing to have been in the Downs. The fort of Richborough, from the similarity of the remains of it to those of Reculver, seems to have been built about the same time, and by the same emperer, Serveris, about the year 205. It stands on the high hill, close to a deep precipice eastward, at the soot of which was the haven. In this fortress, so peculiarly strengthened by its situation, the Romans had afterwards a stationary garrison, and here they had likewise a pharos, of watch tower, the like as at Reculver and other places on this coast, as well to guide the shipping into the haven, as to give notice of the approach of enemies. It is by most supposed that there was, in the time of the Romans, near the fort, in like manner as at Reculver, a city or town, on the decline of the hill, south-westward from it, according to custom, at which a colony was settled by them. Prolemy, in his geography, reckons the city Rutpia as one of the three principal cities of Kent. (fn. 10) Orosius. and Bede too, expressly mention it as such; but when the haven decayed, and there was no longer a traffic and resort to this place, the town decayed likewise, and there have not been, for many ages since, any remains whatever of it left; though quantities of coins and Roman antiquities have been sound on the spot where it is supposed to have once stood.

 

During the latter part of the Roman empire, when the Saxons prevented all trade by sea, and insefted these coasts by frequent robberies, the second Roman legion, called Augusta, and likewise Britannica, which had been brought out of Germany by the emperor Claudius, and had resided for many years at the Isca Silurum, in Wales, was removed and stationed here, under a president or commander, præpositus, of its own, who was subordinate to the count of the Saxon shore, and continued so till the final departure of the Romans from Britain, in the year 410, when this fortress was left in the hands of the Britons, who were afterwards dispossessed of it by the Saxons, during whose time the harbour seems to have began to decay and to swerve up, the sea by degrees entirely deserting it at this place, but still leaving one large and commodious at Sandwich, which in process of time became the usual resort for shipping, and arose a flourishing harbour in its stead, as plainly appears by the histories of those times, by all of which, both the royal Saxon fleets, as well as those of the Danes, are said to sail for the port of Sandwich, and there to lie at different times; (fn. 11) and no further mention is made by any of them of this of Rutupiæ, Reptachester, or Richborough; so that the port being thus destroyed, the town became neglected and desolate, and with the castle sunk into a heap of ruins. Leland's description of it in king Henry VIII.'s reign, is very accurate, and gives an exceeding good idea of the progressive state of its decay to that time. He says, "Ratesburg otherwyse Richeboro was, of ever the ryver of Sture dyd turn his botom or old canale, withyn the Isle of the Thanet, and by Iykelyhod the mayn se came to the very foote of the castel. The mayn se ys now of yt a myle by reason of wose, that has there swollen up. The scite of the town or castel ys wonderful fair apon an hille. The walles the wich remayn ther yet be in cumpase almost as much as the tower of London. They have bene very hye thykke stronge and wel embateled. The mater of them is flynt mervelus and long brykes both white and redde after the Britons fascion. The sement was made of se sand and smaul pible. Ther is a great lykelyhod that the goodly hil abowte the castel and especially to Sandwich ward hath bene wel inhabited. Corne groweth on the hille yn bene mervelous plenty and yn going to plowgh ther hath owt of mynde fownd and now is mo antiquities of Romayne money than yn any place els of England surely reason speketh that this should be Rutupinum. For byside that the name sumwhat toucheth, the very near passage fro Cales Clyves or Cales was to Ratesburgh and now is to Sandwich, the which is about a myle of; though now Sandwich be not celebrated by cawse of Goodwine sandes and the decay of the haven. Ther is a good flyte shot of fro Ratesburg toward Sandwich a great dyke caste in a rownd cumpas as yt had bene for sens of menne of warre. The cumpase of the grownd withyn is not much above an acre and yt is very holo by casting up the yerth. They cawle the place there Lytleborough. Withyn the castel is a lytle paroche chirch of St. Augustine and an heremitage. I had antiquities of the heremite the which is an industrious man. Not far fro the hermitage is a cave wher men have sowt and digged for treasure. I saw it by candel withyn, and ther were conys. Yt was so straite that I had no mynd to crepe far yn. In the north side of the castel ys a hedde yn the walle, now fore defaced with wether. They call it queen Bertha hedde. Nere to that place hard by the wal was a pot of Romayne mony sownd."

 

The ruins of this antient castle stand upon the point of a hill or promontory, about a mile north-west from Sandwich, overlooking on each side, excepting towards the west, a great flat which appears by the lowness of it, and the banks of beach still shewing themselves in different places, to have been all once covered by the sea. The east side of this hill is great part of it so high and perpendicular from the flat at the foot of it, where the river Stour now runs, that ships with the greatest burthen might have lain close to it, and there are no signs of any wall having been there; but at the north end, where the ground rises into a natural terrace, so as to render one necessary, there is about 190 feet of wall left. Those on the other three sides are for the most part standing, and much more entire than could be expected, considering the number of years since they were built, and the most so of any in the kingdom, except Silchester. It is in shape an oblong square, containing within it a space of somewhat less than five acres. They are in general about ten feet high within, but their broken tops shew them to have been still higher. The north wall, on the outside, is about twice as high as it is within, or the other two, having been carried up from the very bottom of the hill, and it seems to have been somewhat longer than it is at present, by some pieces of it sallen down at the east end. The walls are about eleven feet thick. In the middle of the west side is the aperture of an entrance, which probably led to the city or town, and on the north side is another, being an entrance obliquely into the castle. Near the middle of the area are the ruins of some walls, full of bushes and briars, which seem as if some one had dug under ground among them, probably where once stood the prætorium of the Roman general, and where a church or chapel was afterwards erected, dedicated to St. Augustine, and taken notice of by Leland as such in his time. It appears to have been a chapel of ease to the church of Ash, for the few remaining inhabitants of this district, and is mentioned as such in the grant of the rectory of that church, anno 3 Edward VI. at which time it appears to have existed. About a furlong to the south, in a ploughed field, is a large circular work, with a hollow in the middle, the banks of unequal heights, which is supposed to have been an amphitheatre, built of turf, for the use of the garrison, the different heights of the banks having been occasioned by cultivation, and the usual decay, which must have happened from so great a length of time. These stations of the Romans, of which Richborough was one, were strong fortifications, for the most part of no great compass or extent, wherein were barracks for the loding of the soldiers, who had their usual winter quarters in them. Adjoining, or at no great distance from them, there were usually other, buildings forming a town; and such a one was here at Richborough, as has been already mentioned before, to which the station or fort was in the nature of a citadel, where the soldiers kept garrison. To this Tacitus seems to allude, when he says, "the works that in time of peace had been built, like a free town, not far from the camp, were destroyed, left they should be of any service to the enemy." (fn. 12) Which in great measure accounts for there being no kind of trace or remains left, to point out where this town once stood, which had not only the Romans, according to the above observation, but the Saxons and Danes afterwards, to carry forward at different æras the total destruction of it.

 

The burial ground for this Roman colony and station of Richborough, appears to have been on the hill at the end of Gilton town, in this parish, about two miles south-west from the castle, and the many graves which have been continually dug up there, in different parts of it, shew it to have been of general use for that purpose for several ages.

 

The scite of the castle at Richborough was part of the antient inheritance of the family of the Veres, earls of Oxford, from which it was alienated in queen Elizabeth's reign to Gaunt; after which it passed, in like manner as Wingham Barton before-described, to Thurbarne, and thence by marriage to Rivett, who sold it to Farrer, from whom it was alienated to Peter Fector, esq. of Dover, the present possessor of it. In the deed of conveyance it is thus described: And also all those the walls and ruins of the antient castle of Rutupium, now known by the name of Richborough castle, with the scite of the antient port and city of Rutupinum, being on and near the lands before-mentioned. About the walls of Richborough grows Fæniculum valgare, common fennel, in great plenty.

 

It may be learned from the second iter of Antonine's Itinerary, that there was once a Roman road, or highway from Canterbury to the port of Richborough, in which iter the two laft stations are, from Durovernum, Canterbury, to Richborough, ad portum Rutupis, xii miles; in which distance all the different copies of the Itinerary agree. Some parts of this road can be tracted at places at this time with certainty; and by the Roman burial-ground, usually placed near the side of a high road, at Gilton town, and several other Roman vestigia thereabouts, it may well be supposed to have led from Canterbury through that place to Richborough, and there is at this time from Goldston, in Ash, across the low-grounds to it, a road much harder and broader than usual for the apparent use of it, which might perhaps be some part of it.

 

Charities.

A person unknown gave four acres and an half of land, in Chapman-street, of the annual produce of 5l. towards the church assessments.

 

Thomas St. Nicholas, esq. of this parish, by deed about the year 1626, gave an annuity of 11. 5s. to be paid from his estate of Hoden, now belonging to the heirs of Nathaniel Elgar, esq. to be distributed yearly, 10s. to the repairing and keeping clean the Toldervey monument in this church, and 15s. on Christmas-day to the poor.

 

John Proude, the elder, of Ash, yeoman, by his will in 1626, ordered that his executor should erect upon his land adjoining to the church-yard, a house, which should be disposed of in future by the churchwardens and overseers, for a school-house, and for a storehouse, to lay in provision for the church and poor. This house is now let at 1l. per annum, and the produce applied to the use of the poor.

 

Richard Camden, in 1642, gave by will forty perches of land, for the use of the poor, and of the annual produce of 15s. now vested in the minister and churchwardens.

 

Gervas Cartwright, esq. and his two sisters, in 1710 and 1721, gave by deed an estate, now of the yearly value of 50l. for teaching fifty poor children to read, write, &c. vested in the minister, churchwardens, and other trustees.

 

The above two sisters, Eleanor and Anne Cartwright, gave besides 100l. for beautifying the chancel, and for providing two large pieces of plate for the communion service; and Mrs. Susan Robetts added two other pieces of plate for the same purpose.

 

There is a large and commodious workhouse lately built, for the use of the poor, to discharge the expence of which, 100l. is taken yearly out of the poor's rate, till the whole is discharged. In 1604, the charges of the poor were 29l. 15s. 11d. In 1779. 1000l.

 

There is a charity school for boys and girls, who are educated, but not cloathed.

 

The poor constantly relieved are about seventy-five, casually fifty-five.

 

This parish is within the ecclesiastical jurisdiction of the dioceseof Canterbury, and deanry of Bridge.

 

The church, which is dedicated to St. Nicholas, is a handsome building, of the form of a cross, consisting of two isles and two chancels, and a cross sept, having a tall spire steeple in the middle, in which are eight bells and a clock. It is very neat and handsome in the inside. In the high or south chancel is a monument for the Roberts's, arms, Argent, three pheons, sable, on a chief of the second, a greybound current of the first; another for the Cartwrights, arms, Or, a fess embattled, between three catherine wheels, sable. In the north wall is a monument for one of the family of Leverick, with his effigies, in armour, lying cross-legged on it; and in the same wall, westward, is another like monument for Sir John Goshall, with his effigies on it, in like manner, and in a hollow underneath, the effigies of his wife, in her head-dress, and wimple under her chin. A gravestone, with an inscription, and figure of a woman with a remarkable high high-dress, the middle part like a horseshoe inverted, for Jane Keriell, daughter of Roger Clitherow. A stone for Benjamin Longley, LL. B. minister of Ash twenty-nine years, vicar of Eynsford and Tonge, obt. 1783. A monument for William Brett, esq. and Frances his wife. The north chancel, dedicated to St. Nicholas, belongs to the manor of Molland. Against the north wall is a tomb, having on it the effigies of a man and woman, lying at full length, the former in armour, and sword by his side, but his head bare, a collar of SS about his neck, both seemingly under the middle age, but neither arms nor inscription, but it was for one of the family of Harflete, alias Septvans; and there are monuments and several memorials and brasses likewise for that family. A memorial for Thomas Singleton, M. D. of Molland, obt. 1710. One for John Brooke, of Brookestreet, obt. 1582, s. p. arms, Per bend, two eagles.—Several memorials for the Pekes, of Hills-court, and for Masters, of Goldstone. A monument for Christopher Toldervy, of Chartham, obt. 1618. A memorial for Daniel Hole, who, as well as his ancestors, had lived upwards of one hundred years at Goshall, as occupiers of it. In the north cross, which was called the chapel of St. Thomas the Martyr, was buried the family of St. Nicholas. The brass plates of whom, with their arms, are still to be seen. A tablet for Whittingham Wood, gent. obt. 1656. In the south cross, a monument for Richard Hougham, gent. of Weddington, and Elizabeth his wife, daughter of Edward Sanders, gent. of Norborne. An elegant monument for Mary, wife of Henry Lowman, esq. of Dortnued, in Germany. She died in 1737, and he died in 1743. And for lieutenant colonel Christopher Ernest Kien, obt. 1744, and Jane his wife, their sole daughter and heir, obt. 1762, and for Evert George Cousemaker, esq. obt. 1763, all buried in a vault underneath, arms, Or, on a mount vert, a naked man, bolding a branch in his hand, proper, impaling per bend sinister, argent and gules, a knight armed on borjeback, holding a tilting spear erect, the point downwards, all counterchanged. On the font is inscribed, Robert Minchard, arms, A crescent, between the points of it a mullet. Several of the Harfletes lie buried in the church-yard, near the porch, but their tombs are gone. On each side of the porch are two compartments of stone work, which were once ornamented with brasses, most probably in remembrance of the Harfleets, buried near them. At the corner of the church-yard are two old tombs, supposed for the family of Alday.

 

In the windows of the church were formerly several coats of arms, and among others, of Septvans, alias Harflete, Notbeame, who married Constance, widow of John Septvans; Brooke, Ellis, Clitherow, Oldcastle, Keriell, and Hougham; and the figures of St. Nicholas, Keriell, and Hougham, kneeling, in their respective surcoats of arms, but there is not any painted glass left in any part of the church or chancels.

 

John Septvans, about king Henry VII.'s reign, founded a chantry, called the chantry of the upper Hall, as appears by the will of Katherine Martin, of Faversham, sometime his wife, in 1497. There was a chantry of our blessed Lady, and another of St. Stephen likewise, in it; both suppressed in the 1st year of king Edward VI. when the former of them was returned to be of the clear yearly certified value of 15l. 11s. 1½d. (fn. 13)

 

The church of Ash was antiently a chapel of east to that of Wingham, and was, on the foundation of the college there in 1286, separated from it, and made a distinct parish church of itself, and then given to the college, with the chapels likewise of Overland and Fleet, in this parish, appurtenant to this church; which becoming thus appropriated to the college, continued with it till the suppression of it in king Edward VI.'s reign, when this part of the rectory or parsonage appropriate, called Overland parsonage, with the advowson of the church, came, with the rest of the possessions of the college, into the hands of the crown, where the advowson of the vicarage, or perpetual curacy of it did not remain long, for in the year 1558, queen Mary granted it, among others, to the archbishop. But the above-mentioned part of the rectory, or parsonage appropriate of Ash, with those chapels, remained in the crown, till queen Elizabeth, in her 3d year, granted it in exchange to archbishop Parker, who was before possessed of that part called Goldston parsonage, parcel of the late dissolved priory of St. Gregory, by grant from king Henry VIII. so that now this parish is divided into two distinct parsonages, viz. of Overland and of Goldston, which are demised on separate beneficial leases by the archbishop, the former to the heirs of Parker, and the latter, called Gilton parsonage, from the house and barns of it being situated in that hamlet, to George Gipps, esq. M. P. for Canterbury. The patronage of the perpetual curacy remains parcel of the possessions of the see of Canterbury.

 

¶At the time this church was appropriated to the college of Wingham, a vicarage was endowed in it, which after the suppression of the college came to be esteemed as a perpetual curacy. It is not valued in the king's books. The antient stipend paid by the provost, &c. to the curate being 16l. 13s. 4d. was in 1660, augmented by archbishop Juxon with the addition of 33l. 6s. 8d. per annum; and it was afterwards further augmented by archbishop Sheldon, anno 28 Charles II. with twenty pounds per annum more, the whole to be paid by the several lessees of these parsonages. Which sum of seventy pounds is now the clear yearly certified value of it. In 1588 here were communicants five hundred; in 1640, eight hundred and fifty. So far as appears by the registers, the increase of births in this parish is almost double to what they were two hundred years ago.

 

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