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This is a Kinetic Photograph which includes Poe, one of my cats; some of my furniture; a candle; a lamp; and my television screen. Viewed at original size it's a hoot!
One shot SOOC.
Want more? See my new set, "Drawing with Light:"
www.flickr.com/photos/motorpsiclist/sets/72157630589237982/
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Kinetic: Relating to, caused by, or producing motion.
These are called “Kinetic” photographs because there is motion, energy, and movement involved, specifically my and the camera’s movements.
I choose a light source and/or subject, set my camera for a long exposure (typically around 4 seconds), focus on my subject and push the shutter button. When the shutter opens I move the camera around with my hands...large, sweeping, dramatic movements. And then I will literally throw the camera several feet up into the air, most times imparting a spinning or whirling motion to it as I hurl it upward. I may throw the camera several times and also utilize hand-held motion several times in one photo. None of these are Photoshopped, layered, or a composite photo...what you see occurs in one shot, one take.
Aren’t I afraid that I will drop and break my camera? For regular followers of my photostream and this series you will know that I have already done so. This little camera has been dropped many times, and broken once when dropped on concrete outside. It still functions...not so well for regular photographs, but superbly for more kinetic work.
To read more about Kinetic Photography click the Wikipedia link below:
en.wikipedia.org/wiki/Kinetic_photography
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Albeit supremely risky this is one of my favorite ways to produce abstract photographs.
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My photographs and videos and any derivative works are my private property and are copyright © by me, John Russell (aka “Zoom Lens”) and ALL my rights, including my exclusive rights, are reserved. ANY use without my permission in writing is forbidden by law.
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.
Stourhead (/ˈstɑːˌhɛd/[1]) is a 1,072-hectare (2,650-acre) estate[2] at the source of the River Stour near Mere, Wiltshire, England. The estate includes a Palladian mansion, the village of Stourton, gardens, farmland, and woodland. Stourhead is part owned with the National Trust since 1946.
Contents [hide]
1History
2Gardens
2.1Architects
2.2"The Genius of the Place"
3Prints
4Trivia
5Gallery
6References
7External links
History[edit]
The Stourton family, the Barons of Stourton, had lived in the Stourhead estate for 500 years[3] until they sold it to Sir Thomas Meres in 1714.[4] His son, John Meres, sold it to Henry Hoare I, son of wealthy banker Sir Richard Hoare in 1717.[5] The original manor house was demolished and a new house, one of the first of its kind, was designed by Colen Campbell and built by Nathaniel Ireson between 1721 and 1725.[6] Over the next 200 years the Hoare family collected many heirlooms, including a large library and art collection. In 1902 the house was gutted by fire but many of the heirlooms were saved, and the house was rebuilt in a near identical style.[7]
The last Hoare family member to own the property, Henry Hugh Arthur Hoare, gave the house and gardens to the National Trust in 1946, one year before his death; his sole heir and son, Captain "Harry" Henry Colt Arthur Hoare, of the Queen's Own Dorset Yeomanry, had died of wounds received at the Battle of Mughar Ridge on 13 November 1917 in World War I.[7] The last Hoare family member to be born at the house was Edward Hoare on 11 October 1949.
Gardens[edit]
Architects[edit]
Although the main design for the estate at Stourhead was created by Colen Campbell, there were various other architects involved in its evolution through the years. William Benson, Henry Hoare's brother-in-law, was in part responsible for the building of the estate in 1719.[8] Francis Cartwright, a master builder and architect, was established as a "competent provincial designer in the Palladian manner."[9] He worked on Stourhead between the years of 1749–1755. Cartwright was a known carver, presumably of materials such as wood and stone. It is assumed that his contribution to Stourhead was in this capacity. Nathaniel Ireson is the master builder credited for much of the work on the Estate. It is this work that established his career, in 1720.[10]
The original estate remained intact, though changes and additions were made over time. Henry Flitcroft built three temples and a tower on the property. The Temple of Ceres was added in 1744, followed by the Temple of Hercules in 1754 and the Temple of Apollo in 1765. That same year he designed Alfred's Tower, but it wasn't built until 1772.[11] In 1806, the mason and surveyor John Carter added an ornamental cottage to the grounds; at the request of Sir Richard Colt Hoare.[12] The architect William Wilkins created a Grecian style lodge in 1816; for Sir R. Colt Hoare.[12]
In 1840, over a century after the initial buildings were constructed, Charles Parker was hired by Sir Hugh Hoare to make changes to the estate. A portico was added to the main house, along with other alterations. The design of the additions was in keeping with original plans.[13]
"The Genius of the Place"[edit]
The lake at Stourhead is artificially created. Following a path around the lake is meant to evoke a journey similar to that of Aeneas's descent in to the underworld.[14] In addition to Greek mythology, the layout is evocative of the "genius of the place", a concept made famous by Alexander Pope. Buildings and monuments are erected in remembrance of family and local history. Henry Hoare was a collector of art– one of his pieces was Claude Lorrain's Aeneas at Delos, which is thought to have inspired the pictorial design of the gardens.[14] Passages telling of Aeneas's journey are quoted in the temples surrounding the lake.
Monuments are used to frame one another; for example the Pantheon designed by Flitcroft entices the visitor over, but once reached, views from the opposite shore of the lake beckon.[15] The use of the sunken path allows the landscape to continue on into neighbouring landscapes, allowing the viewer to contemplate all the surrounding panorama. The Pantheon was thought to be the most important visual feature of the gardens. It appears in many pieces of artwork owned by Hoare, depicting Aeneas's travels.[16] The plantings in the garden were arranged in a manner that would evoke different moods, drawing visitors through realms of thought.[15] According to Henry Hoare, 'The greens should be ranged together in large masses as the shades are in painting: to contrast the dark masses with the light ones, and to relieve each dark mass itself with little sprinklings of lighter greens here and there.'[17]
View taken from the Grotto, of the lake in autumn colours
Stourhead's lake and foliage as seen from a high hill vantage point
The gardens were designed by Henry Hoare II and laid out between 1741 and 1780 in a classical 18th-century design set around a large lake, achieved by damming a small stream. The inspiration behind their creation were the painters Claude Lorrain, Poussin, and, in particular, Gaspard Dughet, who painted Utopian-type views of Italian landscapes. It is similar in style to the landscape gardens at Stowe.
Included in the garden are a number of temples inspired by scenes of the Grand Tour of Europe. On one hill overlooking the gardens there stands an obelisk and King Alfred's Tower, a 50-metre-tall, brick folly designed by Henry Flitcroft in 1772; on another hill the temple of Apollo provides a vantage point to survey the magnificent rhododendrons, water, cascades and temples. The large medieval Bristol High Cross was moved from Bristol to the gardens. Amongst the hills surrounding the site there are also two Iron Age hill forts: Whitesheet Hill and Park Hill Camp. The gardens are home to a large collection of trees and shrubs from around the world.
Richard Colt Hoare, the grandson of Henry Hoare II, inherited Stourhead in 1783.[7] He added the library wing to the mansion,[7] and in the garden was responsible for the building of the boathouse and the removal of several features that were not in keeping with the classical and gothic styles (including a Turkish Tent). He also considerably enhanced the planting – the Temple of Apollo rises from a wooded slope that was planted in Colt Hoare's time. With the antiquarian passion of the times, he had 400 ancient burial mounds dug up to inform his pioneering History of Ancient Wiltshire.
CORPORATE CHAMPIONS VANCOUVER 2011
Photos by Ron Sombilon Gallery
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Shoreditch London Old Street and City Road Silicon Roundabout Major Road Works.
This was due to be completed Autumn 2022 which has been delayed until Early 2024. The project commenced way back in 2019.
This cycle lane change was initially a three-year project. Now Five Years. The road is the inner ring road for London. They have blocked one of the tube entrances which includes the underpass. Ironically, cyclist do not even use this route since they blocked off the backstreets to traffic. They are trying to sabotage London. The situation is disgusting.
Renovations include the new cable tray for speakers, camera-tracking, power, sensors, repainting, floor buffing, projector mounting and screen, signage, patch bay for audio-visual control, dimmable lighting, spotlighting, networking
Tridacna gigas (Linnaeus, 1758) - giant clam (public display, Bailey-Matthews Shell Museum, Sanibel Island, Florida, USA)
Bivalves are bilaterally symmetrical molluscs having two calcareous, asymmetrical shells (valves) - they include the clams, oysters, and scallops. In most bivalves, the two shells are mirror images of each other (the major exception is the oysters). They occur in marine, estuarine, and freshwater environments. Bivalves are also known as pelecypods and lamellibranchiates.
Bivalves are sessile, benthic organisms - they occur on or below substrates. Most of them are filter-feeders, using siphons to bring in water, filter the water for tiny particles of food, then expel the used water. The majority of bivalves are infaunal - they burrow into unlithified sediments. In hard substrate environments, some forms make borings, in which the bivalve lives. Some groups are hard substrate encrusters, using a mineral cement to attach to rocks, shells, or wood.
The fossil record of bivalves is Cambrian to Recent. They are especially common in the post-Paleozoic fossil record.
The bivalve shown above is the shell of a giant clam, Tridacna gigas, which is the largest bivalve species on Earth. Tridacnid bivalves sit on seafloors with their two shells open to expose colorful mantle tissues. Within the clam's mantle, small microbial organisms (zooxanthellae) live in a symbiotic relationship with the host. In tridacnid bivalves, the zooxanthellae are photosynthesizing dinoflagellates (www.daviddarling.info/images/dinoflagellate.gif). The dinoflagellates provide food for the clam, and the clam also obtains food by filter feeding.
---------------
Info. from museum signage: "The giant clam is not only the largest, but the most spectacular of all bivalves. The species may reach in excess of 1.4 meters (4.5 feet) in size and may weigh more than 400 kilos (about 900 pounds). It inhabits the shallow, warm waters of the Southwest Pacific including the Great Barrier Reef. Its colorful, soft mantle harbors microscopic algae that provide part the nourishment to this giant of the reef. The adductor muscle of the giant clam is a much-prized food item in Southeast Asia, where the species is cultivated in marine farms."
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More info. from museum signage: "The giant Tridacna clam of the southwest Pacific may grow to a length of four feet and a weight of 500 pounds. They live upside-down in shallow, coral reef waters with their huge, fleshy mantle exposed to sunlight. Within this colorful, soft organ, the clam farms its own seaweed food, Zooxanthella. Giant clams are vegetarisn and have never eaten fish, crabs or worms, much less humans. No cases of a person being trapped and drowned by a clam have ever been proved. Cuts and bruises have been caused by the sharp edges of young clams."
---------------
Classification: Animalia, Mollusca, Bivalvia, Veneroida, Cardiidae
----------------------
More info. at:
en.wikipedia.org/wiki/Tridacna
and
The Lidl Run Kildare Events 2013 were held at the Curragh Racecourse, Newbridge, Co. Kildare, Ireland on Sunday 12th May 2013. There were three events: a 10KM, a half marathon, and a full marathon. This is a selection of photographs which includes all events. The photographs are taken from the start and finish of the marathon, the finish of the 10KM, and the finish of the half marathon. Due to the large numbers participating we did not manage to photograph everyone - which was not helped by the weather. Congratulations to Jo Cawley and her RunKildare crew for another great event. The weather didn't dampen the spirits of the many happy participants.
Electronic timing was provided by Red Tag Timing [www.redtagtiming.com/]
Overall Race Summary
Participants: There were approximately 3,000 participants over the 3 race events - there were runners, joggers, and walkers participating.
Weather: A cold breezy morning with heavy rain at the start. The weather dried up for the 10KM and the Half Marathon races
Course: This is an undulating course with some good flat stretches on the Curragh.
Viewing this on a smartphone device?
If you are viewing this Flickr set on a smartphone and you want to see the larger version(s) of this photograph then: scroll down to the bottom of this description under the photograph and click the "View info about this photo..." link. You will be brought to a new page and you should click the link "View All Sizes".
Some Useful Links
GPS Garmin Trace of the Kildare Marathon Route: connect.garmin.com/activity/175709313
Homepage of the Lidl Run Kildare Event: www.kildaremarathon.ie/index.html
Facebook Group page of the Lidl Run Kildare Event: www.facebook.com/RunKildare
Boards.ie Athletics Discussion Board pages about the race series: www.boards.ie/vbulletin/showthread.php?t=2056815306
Our photographs from Run Kildare 2012: www.flickr.com/photos/peterm7/sets/72157629707887620/
Our photographs from Run Kildare 2011: www.flickr.com/photos/peterm7/sets/72157626725200956/
A small selection of photographs from Run Kildare 2010: www.flickr.com/photos/peterm7/sets/72157623899845567/ (first event)
Can I use the photograph with the watermark?
Yes! Absolutely - you can post this photograph to your social networks, blogs, micro-blogging, etc.
How can I get a full resolution, no watermark, copy of these photographs?
All of the photographs here on this Flickr set have a visible watermark embedded in them. All of the photographs posted here on this Flickr set are available, free, at no cost, at full resolution WITHOUT watermark. We take these photographs as a hobby and as a contribution to the running community in Ireland. We do not know of any other photographers who operate such a policy. Our only "cost" is our request that if you are using these images: (1) on social media sites such as Facebook, Tumblr, Pinterest, Twitter,LinkedIn, Google+, etc or (2) other websites, web multimedia, commercial/promotional material that you provide a link back to our Flickr page to attribute us. This also extends the use of these images for Facebook profile pictures. In these cases please make a separate wall or blog post with a link to our Flickr page. If you do not know how this should be done for Facebook or other social media please email us and we will be happy to help suggest how to link to us.
Please email petermooney78 AT gmail DOT com with the links to the photographs you would like to obtain a full resolution copy of. We also ask race organisers, media, etc to ask for permission before use of our images for flyers, posters, etc. We reserve the right to refuse a request.
In summary please remember - all we ask is for you to link back to our Flickr set or Flickr pages. Taking the photographs and preparing them for online posting does take a significant effort. We are not posting photographs to Flickr for commercial reasons. If you really like what we do please spread the link around, send us an email, leave a comment beside the photographs, send us a Flickr email, etc.
If you would like to contribute something for your photograph(s)?
Some people offer payment for our photographs. We do not charge for these photographs. We take these photographs as our contribution to the running community in Ireland. If you feel that the photograph(s) you request are good enough that you would pay for their purchase from other photographic providers we would suggest that you can provide a donation to any of the great charities in Ireland who do work for Cancer Care or Cancer Research in Ireland.
I ran in the race - but my photograph doesn't appear here in your Flickr set! What gives?
As mentioned above we take these photographs as a hobby and as a voluntary contribution to the running community in Ireland. Very often we have actually ran in the same race and then switched to photographer mode after we finished the race. Consequently, we feel that we have no obligations to capture a photograph of every participant in the race. However, we do try our very best to capture as many participants as possible. But this is sometimes not possible for a variety of reasons:
►You were hidden behind another participant as you passed our camera
►Weather or lighting conditions meant that we had some photographs with blurry content which we did not upload to our Flickr set
►There were too many people - some races attract thousands of participants and as amateur photographs we cannot hope to capture photographs of everyone
►We simply missed you - sorry about that - we did our best!
You can email us petermooney78 AT gmail DOT com to enquire if we have a photograph of you which didn't make the final Flickr selection for the race. But we cannot promise that there will be photograph there. As alternatives we advise you to contact the race organisers to enquire if there were (1) other photographs taking photographs at the race event or if (2) there were professional commercial sports photographers taking photographs which might have some photographs of you available for purchase. You might find some links for further information above.
Don't like your photograph here?
That's OK! We understand!
If, for any reason, you are not happy or comfortable with your picture appearing here in this photoset on Flickr then please email us at petermooney78 AT gmail DOT com and we will remove it as soon as possible. We give careful consideration to each photograph before uploading.
I want to tell people about these great photographs!
Great! Thank you! The best link to spread the word around is probably www.flickr.com/peterm7/sets
Overnight LEGO announced this amazing new set from the LEGO Ninjago Movie. The set is pack full of details and is the 3rd largest set LEGO have released.
70620 Ninjago City
4867 Pieces
Price AUD499.99
Available 1st September 2017
================================================
Enjoy endless role-play fun in NINJAGO® City, a hugely-detailed 3-level model connected by a sliding elevator. Level 1 features a traditional fish market, house, a bridge over a stream, and a fishing boat. The second level has a modern fashion store, comic book store, crab restaurant with ‘crab-grilling’ function and cash-dispensing ATM. The vertical city is topped off with Lloyd Garmadon and Misako’s apartment, a rooftop sushi bar with sushi conveyor belt, and a radio tower. This action-packed THE LEGO® NINJAGO MOVIE™ set also includes 16 minifigures and Sweep the maintenance robot.
Includes 16 minifigures: Jay, Kai and Lloyd Garmadon (each with new-for-August-2017 high school outfit decoration), Green Ninja Suit, Misako, Jamanakai Villager, Sally, Ivy Walker, Konrad, Severin Black, Tommy, Guy, Juno, Mother Doomsday, Shark Army Gunner and Officer Noonan, plus Sweep the maintenance robot.
Features a 3-level model (each level lifts off for easy play) connected by a sliding elevator, plus a traditional fishing boat.
Level 1 features a bridge, sewer outlet, stream with translucent-blue and translucent-green water elements, sliding elevator with room for a minifigure, traditional fish market with fish and crab elements, house with dining room and bedroom with sliding screen doors and foldout ‘solar panels’, Sweep the maintenance robot's service station with assorted tool elements, and a taxi stand with telephone element.
Level 2 features a modern fashion store with 2 mannequins and assorted NINJAGO® product elements, a construction site with a bonsai tree, a comic book store with brick-built sign, cashier desk, comic book stand with assorted elements including collectible NINJAGO training cards, a crab restaurant with brick-built crab entrance sign and oven with ‘crab-grilling’ function, a cash-dispensing ATM, 15 bank note elements (ATM can dispense up to 13), and a movie poster display stand with 4 interchangeable movie poster elements.
Place the uncooked crab element in the oven, turn the dial and open the oven to reveal a cooked crab element.
Press the handle behind the ATM to dispense bank note elements.
Level 3 features a radio tower, modern rooftop sushi bar with sushi conveyor belt function and brick-built food, bathroom with sliding door, and brick-built puffer fish and squid sculptures, Lloyd Garmadon and Misako's apartment with an opening window, bunk bed, kitchen unit and attic space for the Green Ninja Suit minifigure.
Turn the dial to activate the sushi conveyor belt.
Weapons include Jay's chain with spike and Shark Army Gunner’s fish flame.
Recreate and role-play exciting THE LEGO® NINJAGO® MOVIE™ scenes.
NINJAGO® City measures over 24” (63cm) high, 12” (31cm) wide and 16” (42cm) deep.
Traditional fishing boat measures over 1” (4cm) high, 3” (10cm) long and 1” (3cm) wide.
#RainbowBricks #LEGONinjagoMovie
City Palace, Jaipur, which includes the Chandra Mahal and Mubarak Mahal palaces and other buildings, is a palace complex in Jaipur, the capital of the Rajasthan state, India. It was the seat of the Maharaja of Jaipur, the head of the Kachwaha Rajput clan. The Chandra Mahal palace now houses a museum but the greatest part of it is still a royal residence. The palace complex, which is located northeast of the centre of the grid patterned Jaipur city, incorporates an impressive and vast array of courtyards, gardens and buildings. The palace was built between 1729 and 1732, initially by Sawai Jai Singh II, the ruler of Amber. He planned and built the outer walls, and later additions were made by successive rulers right up to the 20th century. The credit for the urban layout of the city and its structures is attributed to two architects namely, Vidyadar Bhattacharya, the chief architect in the royal court and Sir Samuel Swinton Jacob, apart from the Sawai himself who was a keen architectural enthusiast. The architects achieved a fusion of the Shilpa Shastra of Indian architecture with Rajput, Mughal and European styles of architecture.
The palace complex lies in the heart of Jaipur city, to the northeast of the very centre. The site for the palace was located on the site of a royal hunting lodge on a plain land encircled by a rocky hill range, five miles south of Amber (city). The history of the city palace is closely linked with the history of Jaipur city and its rulers, starting with Maharaja Sawai Jai Singh II who ruled from 1699-1744. He is credited with initiating construction of the city complex by building the outer wall of the complex spreading over many acres. Initially, he ruled from his capital at Amber, which lies at a distance of 11 kilometres from Jaipur. He shifted his capital from Amber to Jaipur in 1727 because of an increase in population and increasing water shortage. He planned Jaipur city in six blocks separated by broad avenues, on the classical basis of principals of Vastushastra and other similar classical treatise under the architectural guidance of Vidyadar Bhattacharya, a man who was initially an accounts-clerk in the Amber treasury and later promoted to the office of Chief Architect by the King.
Following Jaisingh's death in 1744, there were internecine wars among the Rajput kings of the region but cordial relations were maintained with the British Raj. Maharaja Ram Singh sided with the British in the Sepoy Mutiny or Uprising of 1857 and established himself with the Imperial rulers. It is to his credit that the city of Jaipur including all of its monuments (including the City Palace) are stucco painted 'Pink' and since then the city has been called the "Pink City". The change in colour scheme was as an honour of hospitality extended to the Prince of Wales (who later became King Edward VII) on his visit. This colour scheme has since then become a trademark of the Jaipur city.
Man Singh II, the adopted son of Maharaja Madho Singh II, was the last Maharaja of Jaipur to rule from the Chandra Mahal palace, in Jaipur. This palace, however, continued to be a residence of the royal family even after the Jaipur kingdom merged with the Indian Union in 1949 (after Indian independence in August 1947) along with other Rajput states of Jodhpur, Jaisalmer and Bikaner. Jaipur became the capital of the Indian state of Rajasthan and Man Singh II had the distinction of becoming the Rajapramukh (present day Governor of the state) for a time and later was the Ambassador of India to Spain.
Sundown looking across the weald from Devli's Dyke this evening - the Gull crossing the disc of the distorted Sun was a happy coincidence.
Includes:
VH-EBR c/n: 22614 QANTAS
HS-TGF c/n: 22337 Thai Int'l
9V-SQR c/n: 21943 Singapore
N816FT c/n: 22151 Flying Tigers
JA8146 c/n: 22292 All Nippon
VH-ECC c/n: 22615 QANTAS
N1608B c/n: 22302 Braniff
N1607B c/n: 22234 Braniff
N605BN c/n: 21991 Braniff
5A-DIJ c/n: 22105 Libyan Arab
5A-DIK c/n: 22106 Libyan Arab
Location: Everet-Paine Field
Date: 24 September 1980
Step into the past as you explore more than 8,000 acres of beautiful landscapes that include an old farmstead, and habitats ranging from forest and shrub-steppe to grass and wetlands. The historic Folsom Farm interpretive site demonstrates how the landscape was converted into small farms, ranches and communities beginning in the late 1800s. Displays tell the history of farm life. Enjoy the chance to study numerous species of birds and other wildlife, picnic, backpack, horseback ride, mountain bike, or hunt throughout the entire Fishtrap area. Fishing for stocked rainbow trout is popular at Fishtrap Lake and during the winter at Hog Canyon Lake.
Know Before You Go:
-Entire area is open YEAR ROUND.
-There are no facilities or services available, with the exception of one vault toilet at Folsom Farm.
-No Fees.
-Both lakes have concrete boat launches maintained by Washington Department of Fish and Wildlife -- paid in advance parking permit from WDFW is required.
Directions:
Fishtrap is just a 30-mile drive southwest of Spokane, Washington. From Interstate 90, take Exit 254, and then travel east for 1.75 miles to access the public lands.
Point of Interest:
Part of the Channeled Scablands of eastern Washington, this area is named for the trenches and outcrops of ragged, scarred rock interspersed with wet meadows and wheat fields. The Great Missoula Ice Age Floods that scoured the region more than 12,000 years ago carved out this unique landscape.
Contact:
BLM Spokane District Office
1103 N. Fancher Road
Spokane, WA 99212
(509) 536-1200
Thursday at the Goodwood Festival of Speed. A flat display from the Red Arrows on Thursday. Friday's display was cancelled due to the rain/low cloud.
The monument offers many opportunities to explore and discover the secrets of the Sonoran Desert and includes three wilderness areas, the North Maricopa Mountains Wilderness, the South Maricopa Mountains Wilderness, and the Table Top Wilderness. These wilderness areas offer excellent opportunities for solitude and unconfined recreation. The North Maricopa Mountains Wilderness has two hiking and equestrian trails, the 9-mile Margie’s Cove Trail and the 6-mile Brittlebush Trail. The Table Top Wilderness also has two hiking and equestrian trails, the 7-mile Lava Flow Trail and the 3-mile Table Top Trail. A section of the Juan Bautista de Anza National Historic Trail crosses the national monument. This congressionally designated trail parallels the Butterfield Overland Stage Route, the Mormon Battalion Trail, and the Gila Trail. A four-wheel-drive accessible route follows the trail corridor for approximately 10 miles through the national monument.
For more information, visit: www.blm.gov/az/st/en/prog/blm_special_areas/natmon/son_de...
Photo: Bob Wick, BLM California
The Kerala backwaters are a chain of brackish lagoons and lakes lying parallel to the Arabian Sea coast (known as the Malabar Coast) of Kerala state in southern India. The network includes five large lakes linked by canals, both manmade and natural, fed by 38 rivers, and extending virtually half the length of Kerala state. The backwaters were formed by the action of waves and shore currents creating low barrier islands across the mouths of the many rivers flowing down from the Western Ghats range.
The Kerala Backwaters are a network of interconnected canals, rivers, lakes and inlets, a labyrinthine system formed by more than 900 km of waterways, and sometimes compared to the American Bayou. In the midst of this landscape there are a number of towns and cities, which serve as the starting and end points of backwater cruises. National Waterway No. 3 from Kollam to Kottapuram, covers a distance of 205 km and runs almost parallel to the coast line of southern Kerala facilitating both cargo movement and backwater tourism.
The backwaters have a unique ecosystem - freshwater from the rivers meets the seawater from the Arabian Sea. In certain areas, such as the Vembanad Kayal, where a barrage has been built near Kumarakom, salt water from the sea is prevented from entering the deep inside, keeping the fresh water intact. Such fresh water is extensively used for irrigation purposes.
Many unique species of aquatic life including crabs, frogs and mudskippers, water birds such as terns, kingfishers, darters and cormorants, and animals such as otters and turtles live in and alongside the backwaters. Palm trees, pandanus shrubs, various leafy plants and bushes grow alongside the backwaters, providing a green hue to the surrounding landscape.
Vembanad Kayal is the largest of the lakes, covering an area of 200 km², and bordered by Alappuzha (Alleppey), Kottayam, and Ernakulam districts. The port of Kochi (Cochin) is located at the lake's outlet to the Arabian Sea. Alleppey, "Venice of the East", has a large network of canals that meander through the town. Vembanad is India’s longest lake.
HOUSE BOATS
The kettuvallams (Kerala houseboats) in the backwaters are one of the prominent tourist attractions in Kerala. More than 2000 kettuvallams ply the backwaters, 120 of them in Alappuzha. Kerala government has classified the tourist houseboats as Platinum, Gold and silver.
The kettuvallams were traditionally used as grain barges, to transport the rice harvested in the fertile fields alongside the backwaters. Thatched roof covers over wooden hulls, 30 m in length, provided protection from the elements. At some point in time the boats were used as living quarters by the royalty. Converted to accommodate tourists, the houseboats have become floating cottages having a sleeping area, with western-style toilets, a dining area and a sit out on the deck. Most tourists spend the night on a house boat. Food is cooked on board by the accompanying staff – mostly having a flavour of Kerala. The houseboats are of various patterns and can be hired as per the size of the family or visiting group. The living-dining room is usually open on at least three sides providing a grand view of the surroundings, including other boats, throughout the day when it is on the move. It is brought to a standstill at times of taking food and at night. After sunset, the boat crew provide burning coils to drive away mosquitoes. Ketuvallams are motorised but generally proceed at a slow speed for smooth travel. All ketuvallams have a generator and most bedrooms are air-conditioned. At times, as per demand of customers, electricity is switched off and lanterns are provided to create a rural setting.
While many ketuvalloms take tourists from a particular point and bring them back to around the same point next morning there are some specific cruises mostly in the Alappuzha area, such as the one night cruise from Alappuzha to Thotapally via Punnamada Lake two nights cruise from Alappuzha to Alumkavadi,[8] one night cruise from Alappuzha to Kidangara, and one night cruise from Alappuzha to Mankotta. There are numerous such cruises.
Beypore, located 10 km south of Kozhikode at the mouth of the Chaliyar River, is a famous fishing harbour, port and boat building centre. Beypore has a 1,500 year-tradition of boatbuilding. The skill of the local shipwrights and boat builders are widely sought after. There is a houseboat-building yard at Alumkadavu, in Ashtamudi Kayal near Kollam.
FERRY SERVICES
Regular ferry services connect most locations on both banks of the backwaters. The Kerala State Water Transport Department operates ferries for passengers as well as tourists. It is the cheapest mode of transport through the backwaters.
ECONOMIC SIGNIFICANCE
Connected by artificial canals, the backwaters form an economical means of transport, and a large local trade is carried on by inland navigation. Fishing, along with fish curing is an important industry.
Kerala backwaters have been used for centuries by the local people for transportation, fishing and agriculture. It has supported the efforts of the local people to earn a livelihood. In more recent times, agricultural efforts have been strengthened with reclamation of some backwater lands for rice growing, particularly in the Kuttanad area. Boat making has been a traditional craft, so has been the coir industry.
Kuttanad is crisscrossed with waterways that run alongside extensive paddy fields, as well as fields of cassava, banana and yam. A unique feature of Kuttanad is that many of these fields are below sea level and are surrounded by earthen embankments. The crops are grown on the low-lying ground and irrigated with fresh water from canal and waterways connected to Vembanad lake. The area is similar to the dikes of the Netherlands where land has been reclaimed from the sea and crops are grown.
WIKIPEDIA
History of the Vienna Philharmonic
The orchestra of the Vienna Philharmonic was founded on March 28, 1842. It was founded by the German composer Otto Nicolai, whose creations include the opera "The Merry Wives of Windsor". Nearly a century later, the club was dissolved in December 1938 during the Nazi period by the law on the "transfer and incorporation of clubs, organizations and associations" for the time being and the assets fell to the State Theater and the Stage Academy of the City of Vienna. This was, however, a few days later at the urging of the conductor and musicologist Dr. Heinz Drewes largely reversed. Dr. Drewes was the leader of the "entire German musical life" and so he used his influence on the Reich propaganda minister Goebbels. Ultimately, Goebbels decreed in June 1939 that the Vienna Philharmonic as an association should retain their most extensive independence on the condition that the club is subject to his supervision and that the articles of association regarding the National Socialist principles is changed. Thus, the club's assets were released again.
In 1939, the idea of the New Year's Concert, at which time only the music of Johann Strauss was played, was born. This concert series of the New Year's Concert has become one of the cultural highlights of the year and is always broadcast live on television. The magnificent pictures from Vienna are accompanied, among other things, by fantastic flowers and dance performances by the Wiener Ballett. With the end of the Second World War, the Vienna Philharmonic Orchestra once again became completely independent and the orchestra played two major concert evenings right after the liberation of Vienna in April 1945. A special focus is still the position of the conductor at the Vienna Philharmonic. Because until 1933, the orchestra was directed by a single conductor every season. From 1933 there were only guest conductors. Great merits in the early years had especially the conductors Arturo Toscanini from 1933 to 1937 and intermittently from 1933 to 1954 Wilhelm Furtwängler. Herbert von Karajan, Karl Böhm, Paul Hindemith and Daniel Barenboim are among the famous guest conductors. Also as a guest conductor conducted from 1966, the later honorary member Leonard Bernstein repeatedly the orchestra. One of Leonard Bernstein's most outstanding works in collaboration with the Vienna Philharmonic is, for example, the adaptation of the works of Gustav Mahler, who himself had directed the orchestra from 1898 to 1901 for three years as a subscription conductor to the Vienna Philharmonic.
Vienna Philharmonic coins
Appropriately to the Vienna Philharmonic, the Austrian Mint, which mints all coins in Austria, has been issuing a bullion every year since 1989, which after the orchestra precisely is called the Vienna Philharmonic. At first, the coins were pure gold. Since 2008 there is also an annual silver version. Their value does not correspond to the nominal value, but the Vienna Philharmonic is a bullion coin whose value depends on the current precious metal value. The motif of the Vienna Philharmonic is always the same. The front of the Vienna Philharmonic Münze designed by Thomas Pesendorfer shows some of the classical orchestral instruments such as bassoon, horn, harp and four violins, as well as a cello in the middle. The reverse shows the organ, which is located in the Golden Hall of the Wiener Musikverein. Only the respective year is changed. The coin is now available in four sizes. As a special coinage, a 1000-ounce coin, the so-called "Big Phil", was released in 2004 on the occasion of the 15th anniversary, and another coin in 2009 for the 20th anniversary. Both are traded as collectors' items because of the limited edition and are therefore more expensive than the actual precious metal value.
Geschichte der Wiener Philharmoniker
Das Orchester der Wiener Philharmoniker wurde am 28. März 1842 gegründet. Ins Leben gerufen hatte es der deutsche Komponist Otto Nicolai, aus dessen Feder unter anderem die Oper "Die lustigen Weiber von Windsor" stammt. Knapp ein Jahrhundert später wurde der Verein im Dezember 1938 in der NS-Zeit durch das Gesetz zur "Überleitung und Eingliederung von Vereinen, Organisationen und Verbänden" vorerst aufgelöst und das Vermögen fiel dem Staatstheater und der Bühnenakademie der Stadt Wien zu. Dies wurde jedoch wenige Tage später auf Drängen des Dirigenten und Musikwissenschaftlers Dr. Heinz Drewes größtenteils wieder rückgängig gemacht. Dr. Drewes war der Leiter des "gesamten deutschen Musiklebens" und so nutzte er seinen Einfluss auf den Reichspropagandaminister Goebbels. Letztlich verfügte Goebbels im Juni 1939, dass die Wiener Philharmoniker als Verein ihre weitestgehende Selbständigkeit behalten sollten unter der Bedingung, dass der Verein seiner Aufsicht unterstellt wird dass die Vereinssatzung hinsichtlich der nationalsozialistischen Grundsätze geändert wird. Damit wurde auch das Vereinsvermögen wieder frei gegeben.
Im Jahr 1939 entstand zugleich die Idee des Neujahrskonzerts, bei dem damals ausschließlich die Musik von Johann Strauss gespielt wurde. Diese Konzertreihe des Neujahrskonzerts ist inzwischen einer der kulturellen Höhepunkte des Jahres und wird immer live im Fernsehen übertragen. Die prächtigen Bilder aus Wien werden unter anderem untermalt durch phantastische Blumen und Tanzeinlagen des Wiener Balletts. Mit dem Ende des Zweiten Weltkriegs wurde der Verein der Wiener Philharmoniker wieder komplett unabhängig und das Orchester spielte gleich nach der Befreiung von Wien im April 1945 zwei große Konzertabende. Ein ganz besonderer Augenmerk gilt noch der Stelle des Dirigenten bei den Wiener Philharmonikern. Denn bis zum Jahr 1933 wurde das Orchester jede Saison von einem einzigen Dirigenten geleitet. Ab 1933 gab es nur noch Gastdirigenten. Große Verdienste hatten in den Anfangsjahren vor allem die Dirigenten Arturo Toscanini von 1933 bis 1937 und mit Unterbrechungen von 1933 bis 1954 Wilhelm Furtwängler. Zu den berühmten Gastdirigenten zählen unter anderem Herbert von Karajan, Karl Böhm, Paul Hindemith oder Daniel Barenboim. Ebenfalls als Gastdirigent leitete ab 1966 das spätere Ehrenmitglied Leonard Bernstein mehrfach das Orchester. Zu den herausragendsten Werken von Leonard Bernstein in Zusammenarbeit mit den Wiener Philharmonikern zählt beispielsweise die Bearbeitung der Werke von Gustav Mahler, der von 1898 bis 1901 selbst drei Jahre lang als Abonnementdirigent der Wiener Philharmoniker das Orchester geleitet hatte.
Wiener Philharmoniker Münzen
Passend zu den Wiener Philharmonikern gibt die Münze Österreich, die alle Münzen in Österreich prägt, seit dem Jahr 1989 jedes Jahr eine Anlagemünze heraus, die nach dem Orchester eben der Wiener Philharmoniker genannt wird. Zunächst waren die Münzen aus reinem Gold. Seit 2008 gibt es auch eine jährliche Silberversion. Ihr Wert entspricht nicht dem reinen Nennwert, sondern der Wiener Philharmoniker ist eine Bullionmünze, deren Wert sich nach dem aktuellen Edelmetallwert richtet. Das Motiv des Wiener Philharmoniker ist immer gleich. Die Vorderseite der von Thomas Pesendorfer gestalteten Wiener Philharmoniker Münze zeigt einige der klassischen Orchesterinstrumente wie Fagott, Horn, Harfe und dazu vier Geigen sowie in der Mitte ein Cello. Die Rückseite zeigt die Orgel, die sich im Goldenen Saal vom Wiener Musikverein befindet. Geändert wird nur das jeweilige Prägejahr. Die Münze gibt es inzwischen in vier Größen zu kaufen. Als Sonderprägungen erschien 2004 zum 15-jährigen Jubiläum eine 1000-Unzen-Münze, der sogenannte "Big Phil", und 2009 zum 20-jährigen Jubiläum eine weitere Münze. Beide werden wegen der limitierten Auflage als Sammlerobjekte gehandelt und sind daher teurer als der eigentliche Edelmetallwert.
www.geschichte-oesterreich.com/musik/wiener_philharmonike...
International student orientation includes members of the Class of 2018, international transfer students, and international exchange students. Part of their orientation includes a tour of the libraries and an ice cream social. (Photo by Josh Renaud '17)
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Battery Park (also known as The Battery), which includes a park known as White Point Gardens, is a landmark promenade in Charleston, South Carolina famous for its stately antebellum homes. First used as a public park in 1837, it became a place for artillery during the American Civil War. It stretches along the shores of the Charleston peninsula, bordered by the Ashley and Cooper Rivers. Fort Sumter is visible from the Cooper River side and the point, as is Castle Pinckney, the World War II aircraft carrier USS Yorktown (CV-10), Fort Moultrie, and Sullivan's Island.
In the 18th century, rocks and heavy materials were used to fortify the shore of the Cooper River. In 1838, this area of the Battery, known as High Battery, became a promenade.
Before becoming a park, Fort Broughton (ca. 1735) and Fort Wilkins (during the American Revolution and War of 1812) occupied White or Oyster Point, so named because of the piles of bleached oyster shells on the point. This site is now known as White Point Garden(s) and boasts many large oak trees, a bandstand, a few memorials, and pieces of artillery, some of which were used during the United States Civil War.
A monument in White Point Gardens commemorates the hanging near that site of pirate captain Stede Bonnet and his crew in 1718, as well as the 1719 hanging of Richard Worley's pirates. The monument states that 29 of Bonnet's crew were executed close by. Although 29 of Bonnet's crew were sentenced to death, the evidence suggests that only 22 were actually hanged.
Includes front entrance, information desk, historic weaponry section, museum shop and cafe, and a rear exit
Includes home fries and fresh fruit. Extra side of bacon. Photo credit: Nancy Wong Photo taken: Apr.25,2015
FMA Vancouver
photos by Ron Sombilon Gallery
FMA 2008 promo trailer
www.FMAvancouver.com/2008promo
This Charity Benefitting Concert Gala is the premier red carpet event of Western Canada. Not just a fashion show, not just a concert, FMA Vancouver is a fusion of catwalk and concert set against the backdrop of one of the world’s most beautiful and trend setting cities.
Canadian comedian and actress Ellie Harvie and ET Canada’s Erin Cebula are hosting this year’s FMA Vancouver. The media duo will present 'Sky 360', the airy incarnation of fashion runway, live music and art performance held on September 27, 2008 at The Centre in Vancouver for the Performing Arts. Sky 360 re-lives the old world glamour of travel as each segment celebrates the excitement of jet-setting and far away destinations along with an eco-green theme.
The whole venue at The Centre will be transformed into an exhilarating airport scene with staff in ’60s and ’70s-inspired airline uniforms designed by Jolie Chan of Jolie Couture.
Terminal 1 – Trans Canada - an exclusively Canadian roster of designers, musicians and artists.
Terminal 2 – Mile High - a provocative selection of lingerie and bathing suits.
Terminal 3 – Eco Green - featuring designers who are taking eco-couture to the next level.
Terminal 4 – Elite Star - first class finale of high profile designers.
International designers include Betsey Johnson, Wolford and Calvin Klein, while national stars join their ranks such as TV’s 'Making it Big' winner Jason Matlo, Bikini-designer extraordinaire, Anna Kosturova, Canada’s Project Runway designer judge Shawn Hewson's 'Bustle', winner Evan Biddell, and runner-up Carlie Wong. Further locally-based stars include Nicole Bridger, Elroy Apparel, Evan & Dean, Odd Molly, Jacqueline Conoir and Mellinda Mae Harlingten. Also featuring top graduates from Kwantlen University College and Helen Lefeaux School of Fashion Design.
This year’s beneficiary is the Canadian Make Poverty History as part of Bono and Bob Geldof's international campaign to eradicate global poverty, and The WordLoveWorldLove Project that connects Canadian children with children in developing countries who have been impacted by crisis.
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www.vapestore.wupples.com/index.php/2016/06/06/10-best-di...
Location
Eastern side of the Civic centre, accessible from Coranderrk, Ballumbir, Akuna and Bunda Streets.
Facilities
Facilities include: Rotunda; barbecues; children's playgrounds; picnic areas; and a public toilet in the centre of the park. Time controlled parking is available outside the park only.
History
Glebe Park is an important green sanctuary in the city. Its mature trees and its distinctive stone and steel picket fences set it apart from all other parks in Canberra. For office workers, shoppers, tourists, including the many who visit the adjacent National Convention Centre, and the residents of nearby Reid, it is Civic's most accessible park.
A part of Canberra's history
The park is but a small part of a 40 hectare glebe which, together with a nearby area of approximately 0.8 hectares, was transferred by merchant and pastoralist Robert Campbell to the Church of England in the early 1840s when the area was known as "Canberry". On the smaller site was built St Johns Church, which has continued to the present day serving its parish community. The glebe, later expanded to 47 hectares, was for a parsonage and for the parson's use as a farm.
The subsequent planting of trees was to lead, a century later, to a community campaign to save those trees and their descendants by creating a public park there. That park was officially defined and named on 14 December 1983. Its future was assured by National Trust (ACT) and Australian Heritage Commission listings. After construction by the National Capital Development Commission between 1983 and 1988 it was officially opened on Canberra Day March 12 1989.
A heritage influenced design
In keeping with the historic background of the existing trees and their informal character the park has been designed to reflect the character of a traditional English park. The park's borders that front roads are marked by a stone fence with steel railings, while access is gained through formal gateways. The park is criss-crossed with paved paths. Each of the ten gates are officially named to reflect the historic background of the area since European settlement. Names include St John's, Galliad Smith, Campbell and Canberry.
The mature trees of the park create a relaxed atmosphere much sought after in the heart of the city. The blaze of autumn colour diffused with sunlight marks the change of the seasons in a way seldom experienced in other Canberra parks. Of the park's 663 trees 508 are English elms (Ulmus procera) and 92 are English oaks (Quercus robur).
A 19th century style rotunda, a children's playground and a large sculpture depicting "Egle, the Queen of Serpants" donated by the Lithuanian community in Australia, add interest to the park. United Nations Day in 1989 and the Diamond Jubilee of the Horticulture Society of Canberra (1929-1989) are commemorated with tree plantings.
A popular inner city park
Glebe Park is well used throughout the week and weekend during daylight hours, particularly in the spring, summer and autumn. Groups congregate around the barbecues and the children's playground.
The park has become a popular venue for organised events such as weddings, public meetings and concerts for which a permit may be required, while it is an excellent venue for large festivals. During March it is used for a wide range of events during the Canberra Festival, including the ever popular Canberra Times Art Show.
During a visit to Glebe Park reflect on the events over the past 150 years which have contributed to the evolution of the park and today's Canberra.
Reference
Gray, J (1997) The Historical and Cultural Background of selected Urban Parks in Canberra.
Source: www.tams.act.gov.au/play/pcl/parks_reserves_and_open_plac...
Northwest Airlines began life in September 1926 as Northwest Airways, headquartered in Detroit, Michigan and flying air mail. A year later, it expanded its service to include passenger routes, flying Hamilton H-47 biplanes. Due to the fallout from the Air Mail Scandal of the early 1930s, Northwest Airways changed its name to Northwest Airlines in 1934 to distance itself from its air mail beginnings. By that time, it had already moved its main base of operations to Minneapolis-St. Paul, Minnesota, and was operating a comparatively large route network through the upper Midwest. Due to this experience, Northwest got the coveted route from New York to Seattle, making the airline one of the few transcontinental American airlines. Because a good deal of this route was flown over the rugged Rocky Mountains in often winter weather, Northwest pioneered long-distance mountain flying in poor conditions.
During World War II, Northwest’s experience in flying these routes served it well: many of its pilots were tapped to map out the Alaska-Siberia (ALSIB) air ferrying route from Great Falls, Montana to destinations in the Soviet Union. With the risk of crashing into sparsely populated areas a real threat, Northwest’s aircraft were painted with bright red tails to better find them if there was a crash-landing. When the war ended, Northwest kept their red tails, which brought recognition from potential passengers. It also gained the airline’s pilots a great deal of experience in long-distance flight.
Before the war, Northwest was already considering a transpacific route through Alaska and Japan to China; after the war, with new long-range aircraft such as the Douglas DC-4 and Boeing 377 Stratocruiser becoming available, this idea became a reality. Northwest flew its first transpacific route from Minneapolis to Tokyo in 1947—the first to use the “Great Northern Circle” route. Asia became Northwest’s stock in trade after 1947. To reflect this, the airline began calling itself Northwest Orient, though it did not begin applying this title to its aircraft immediately. For awhile, Northwest was not only one of the more well-known American air carriers, it was also Japan’s largest and the American airline with the most destinations in Canada.
By 1960, when Northwest received its first jets (Douglas DC-8s, though these were soon replaced by Boeing 707s), it had the most Asian destinations of any US airline, and was also the largest airline in the Pacific Northwest as well, with a dense network serving small airports between Seattle and Minneapolis, as well a few Midwest locations as well. It had also acquired turboprops as one of the launch customers for the Lockheed L-188 Electra, but after a series of catastrophic accidents, these were quietly replaced by Boeing 727s, making Northwest one of the first all-jet airlines. A new livery was adopted in the early 1970s that kept the red tail but dropped the words “Northwest”; new titling with “Northwest Orient” was carried on the forward fuselage, and more bare metal was used. About the same time, Northwest entered the wide-body field in a big way, ordering both Boeing 747s and McDonnell Douglas DC-10s. In 1977, it received its first European routes, making it a worldwide airline.
Because of its extensive international network and near-stranglehold on the Pacific Northwest (its only rival was Western Airlines), Northwest weathered the post-deregulation American market and even profited from it: seeking to expand into the American East and South, it bought Republic Airlines in 1986. Not long afterwards, the title “Orient” was dropped from Northwest’s advertising and aircraft, as it was no longer a primarily transpacific airline.
This was not without price, however: the sudden acquisition of Republic left Northwest glutted with aircraft it could not afford to operate and routes it did not want, while continued issues with labor nearly led to strikes. The airline nearly went bankrupt in 1993 before restructuring; a modernization program began, with many regional routes farmed out to Northwest Airlink, its commuter service, and older aircraft leased out. Its European routes, however, were strengthened by a close relationship and codesharing agreement with KLM Royal Dutch Airlines.
Northwest returned to profitability after a brief period of low sales in the late 1990s, but then was deluged with a number of problems. This included its previous uncontested dominance in Asia being challenged by United and Delta; the latter, after buying out Western, was also becoming increasingly present in the Pacific Northwest as well, where low-cost carriers like Alaska and Southwest were beginning to take a toll. Labor issues continued to be an issue as well. After the 9/11 attacks grounded American air traffic—which for Northwest, came on the heels of a strike that grounded the airline for two weeks—Northwest filed for bankruptcy in 2005.
This led to a massive sell-off of older aircraft, the end of a great deal of complimentary items for passengers, slashing its Airlink fleet, and other cost-saving measures. Northwest emerged from bankruptcy in 2007, but never truly recovered. It curtailed some of its European routes in exchange for new routes to China, but though Northwest was posting a profit, it was not the airline giant it had been in the 1980s and 1990s.
In 2008, Northwest announced a merger with Delta, which would allieviate the problems with both airlines, though Northwest was clearly the junior partner. Though Delta adopted a shade of red in its famous widget identical to that of Northwest’s tail colors, the Northwest brand disappeared by 2010 as Delta became the largest airline in the world by fleet size.
I found this Boeing 727 miniature/toy in an antique store in Poulsbo, Washington while on vacation. (They had almost everything Northwest flew in the late 1970s in the same scale...I should've bought all of them!) This is a tiny toy, much smaller than even the AeroMinis that are in the Poletto Collection. It is in Northwest's "Northwest Orient" colors the airline carried through the 1970s and most of the 1980s.
Luxor (Arabic: الأقصر, romanized: al-ʾuqṣur, lit. 'the palaces') is a city in Upper Egypt, which includes the site of the Ancient Egyptian city of Thebes. Luxor had a population of 1,333,309 in 2020, with an area of approximately 417 km2 (161 sq mi) and is the capital of the Luxor Governorate. It is among the oldest inhabited cities in the world.
Luxor has frequently been characterized as the "world's greatest open-air museum", as the ruins of the Egyptian temple complexes at Karnak and Luxor stand within the modern city. Immediately opposite, across the River Nile, lie the monuments, temples and tombs of the west bank Theban Necropolis, which includes the Valley of the Kings and Valley of the Queens. Thousands of tourists from all around the world arrive annually to visit Luxor's monuments, contributing greatly to the economy of the modern city. Yusuf Abu al-Haggag is the patron saint of Luxor.
Etymology
The name Luxor (Arabic: الأقصر, romanized: al-ʾuqṣur, lit. 'the palaces', pronounced /ˈlʌksɔːr, ˈlʊk-/, Egyptian Arabic pronunciation: [ˈloʔsˤoɾ], Upper Egyptian: [ˈloɡsˤor]) derives from the Arabic qasr (قصر), meaning "castle" or "palace". It may be equivalent to the Greek and Coptic toponym τὰ Τρία Κάστρα ta tria kastra and ⲡϣⲟⲙⲧ ⲛ̀ⲕⲁⲥⲧⲣⲟⲛ pshomt enkastron respectively, which both mean "three castles")
The Sahidic Coptic name Pape (Coptic: ⲡⲁⲡⲉ, pronounced Coptic pronunciation: [ˈpapə]), comes from Demotic Ỉp.t "the adyton", which, in turn, is derived from the Egyptian. The Greek forms Ἀπις and Ὠφιεῖον come from the same source. The Egyptian village Aba al-Waqf (Arabic: أبا الوقف, Ancient Greek: Ωφις) shares the same etymology.
The Greek name is Thebes (Ancient Greek: Θῆβαι) or Diospolis. The Egyptian name of the city is Waset, also known as Nut (Coptic: ⲛⲏ)
Luxor was the ancient city of Thebes, the capital of Upper Egypt during the New Kingdom, and the city of Amun, later to become the god Amun-Ra. The city was regarded in the ancient Egyptian texts as wAs.t (approximate pronunciation: "Waset"), which meant "city of the sceptre", and later in Demotic Egyptian as ta jpt (conventionally pronounced as "tA ipt" and meaning "the shrine/temple", referring to the jpt-swt, the temple now known by its Arabic name Karnak, meaning "fortified village"), which the ancient Greeks adapted as Thebai and the Romans after them as Thebae. Thebes was also known as "the city of the 100 gates", sometimes being called "southern Heliopolis" ('Iunu-shemaa' in Ancient Egyptian), to distinguish it from the city of Iunu or Heliopolis, the main place of worship for the god Ra in the north. It was also often referred to as niw.t, which simply means "city", and was one of only three cities in Egypt for which this noun was used (the other two were Memphis and Heliopolis); it was also called niw.t rst, "southern city", as the southernmost of them.
The importance of the city started as early as the 11th Dynasty, when the town grew into a thriving city. Montuhotep II, who united Egypt after the troubles of the First Intermediate Period, brought stability to the lands as the city grew in stature. The Pharaohs of the New Kingdom in their expeditions to Kush, in today's northern Sudan, and to the lands of Canaan, Phoenicia and Syria saw the city accumulate great wealth and rose to prominence, even on a world scale. Thebes played a major role in expelling the invading forces of the Hyksos from Upper Egypt, and from the time of the 18th Dynasty to the 20th Dynasty, the city had risen as the political, religious and military capital of Ancient Egypt.
The city attracted peoples such as the Babylonians, the Mitanni, the Hittites of Anatolia (modern-day Turkey), the Canaanites of Ugarit, the Phoenicians of Byblos and Tyre, the Minoans from the island of Crete. A Hittite prince from Anatolia even came to marry with the widow of Tutankhamun, Ankhesenamun. The political and military importance of the city, however, faded during the Late Period, with Thebes being replaced as political capital by several cities in Northern Egypt, such as Bubastis, Sais and finally Alexandria.
However, as the city of the god Amun-Ra, Thebes remained the religious capital of Egypt until the Greek period. The main god of the city was Amun, who was worshipped together with his wife, the Goddess Mut, and their son Khonsu, the God of the moon. With the rise of Thebes as the foremost city of Egypt, the local god Amun rose in importance as well and became linked to the sun god Ra, thus creating the new 'king of gods' Amun-Ra. His great temple at Karnak, just north of Thebes, was the most important temple of Egypt right until the end of antiquity.
Later, the city was attacked by Assyrian emperor Ashurbanipal who installed a new prince on the throne, Psamtik I. The city of Thebes was in ruins and fell in significance. However, Alexander the Great did arrive at the temple of Amun, where the statue of the god was transferred from Karnak during the Opet Festival, the great religious feast. Thebes remained a site of spirituality up to the Christian era, and attracted numerous Christian monks of the Roman Empire who established monasteries amidst several ancient monuments including the temple of Hatshepsut, now called Deir el-Bahri ("the northern monastery").
Following the Muslim conquest of Egypt, part of the Luxor Temple was converted from a church to a mosque. This mosque is currently known as the Abu Haggag Mosque today.
The 18th century saw an increase of Europeans visiting Luxor, with some publishing their travels and documenting its surroundings, such as Claude Sicard, Granger, Frederick Louis Norden, Richard Pococke, Vivant Denon and others. By the 20th century, Luxor had become a major tourist destination.
Archaeology
In April 2018, the Egyptian Ministry of Antiquities announced the discovery of the shrine of god Osiris- Ptah Neb, dating back to the 25th dynasty in the Temple of Karnak. According to archaeologist Essam Nagy, the material remains from the area contained clay pots, the lower part of a sitting statue and part of a stone panel showing an offering table filled with a sheep and a goose which were the symbols of the god Amun.
On the same day in November 2018, two different discoveries were announced. One was by the Egyptian Supreme Council of Antiquities that had found a 13th-century tomb on the West Bank belonging to Thaw-Irkhet-If, the overseer of the mummification shrine at the temple of Mut, and his wife. Five months of excavation work until this point had revealed colorful scenes of the family and 1,000 funerary statues or ushabti. The other discovery was of 1000 ushabti and two sarcophagi each containing a mummy in the TT33 complex by a joint team from the IFAO (French Institute of Oriental Archaeology, Cairo, Egypt) and the University of Strasbourg. One of the sarcophagi was opened in private by Egyptian antiquities officials, while the other, of a female 18th Dynasty woman named Thuya, was opened in front of international media.
In October 2019, Egyptian archaeologists headed by Zahi Hawass revealed an ancient "industrial area" used to manufacture decorative artefacts, furniture and pottery for royal tombs. The site contained a big kiln to fire ceramics and 30 ateliers. According to Zahi Hawass, each atelier had a different aim – some of them were used to make pottery, others used to produce gold artefacts and others still to churn out furniture. About 75 meters below the valley, several items believed to have adorned wooden royal coffins, such as inlaid beads, silver rings and gold foil were unearthed. Some artefacts depicted the wings of deity Horus.
In October 2019, the Egyptian archaeological mission unearthed thirty well-preserved wooden coffins (3,000 years old) in front of the Mortuary Temple of Hatshepsut in El-Assasif Cemetery. The coffins contained mummies of twenty-three adult males, five adult females and two children, who are believed to be from the middle class. According to Hawass, mummies were decorated with mixed carvings and designs, including scenes from Egyptian gods, hieroglyphs, and the Book of the Dead, a series of spells that allowed the soul to navigate in the afterlife. Some of the coffins had the names of the dead engraved on them.
On the 8th of April 2021, Egyptian archaeologists led by Zahi Hawass found Aten, a 3,400-year-old "lost golden city" near Luxor. It is the largest known city from Ancient Egypt to be unearthed to date. The site was said by Betsy Bryan, professor of Egyptology at Johns Hopkins University to be "the second most important archaeological discovery since the tomb of Tutankhamen". The site is celebrated by the unearthing crew for showing a glimpse into the ordinary lives of living ancient Egyptians whereas past archaeological discoveries were from tombs and other burial sites. Many artefacts are found alongside the buildings such as pottery dated back to the reign of Amenhotep III, rings and everyday working tools. The site is not completely unearthed as of the 10th of April 2021.
Landmarks
West bank
Valley of the Kings
Valley of the Queens
Medinet Habu (Mortuary Temple of Ramesses III, etc.)
The Ramesseum (memorial temple of Ramesses II)
Deir el-Medina (workers' village)
Tombs of the Nobles
Deir el-Bahari (Mortuary Temple of Hatshepsut, etc.)
Malkata (palace of Amenophis III)
Colossi of Memnon (memorial temple of Amenophis III)
Al-Asasif cemetery
East bank
Luxor Temple
Luxor International Airport
Karnak Temple
Luxor Museum
Mummification Museum
Winter Palace Hotel
Climate
Luxor has a hot desert climate (Köppen climate classification BWh) like the rest of Egypt. Aswan and Luxor have the hottest summer days of any other city in Egypt. Aswan and Luxor have nearly the same climate. Luxor is one of the sunniest and driest cities in the world. Average high temperatures are above 40 °C (104 °F) during summer (June, July, August). During the coolest month of the year, average high temperatures remain above 22 °C (71.6 °F) while average low temperatures remain above 5 °C (41 °F).
The climate of Luxor has precipitation levels lower than even most other places in the Sahara, with less than 1 mm (0.04 in) of average annual precipitation. The desert city is one of the driest ones in the world, and rainfall does not occur every year. The air in Luxor is more humid than Aswan but still very dry. There is an average relative humidity of 39.9%, with a maximum mean of 57% during winter and a minimum mean of 27% during summer.
The climate of Luxor is extremely clear, bright and sunny year-round, in all seasons, with a low seasonal variation, with about some 4,000 hours of annual sunshine, very close to the maximum theoretical sunshine duration.
In addition, Luxor, Minya, Sohag, Qena and Asyut have the widest difference of temperatures between days and nights of any city in Egypt, with almost 16 °C (29 °F) difference.
The hottest temperature recorded was on May 15, 1991, which was 50 °C (122 °F) and the coldest temperature was on February 6, 1989, which was −1 °C (30 °F).
Coptic Catholic Eparchy
The Coptic Catholic (Alexandrian Rite) minority established on November 26, 1895 an Eparchy (Eastern Catholic Diocese) of Luqsor (Luxor) alias Thebes, on territory split off from the Apostolic Vicariate of Egypt. Its episcopal see is a St. George cathedral in Luxor.
In turn, it lost territory on August 10, 1947 to establish the Eparchy of Assiut and again on 14 September 1981 to establish Sohag.
Suffragan Eparchs of Luxor
Ignazio Gladès Berzi (March 6, 1896 – died January 29, 1925)
Marc Khouzam (August 6, 1926 – August 10, 1947), also Apostolic Administrator of Alexandria of the Copts (Egypt) (December 30, 1927 – August 10, 1947); later Coptic Catholic Patriarch of Alexandria (10 August 10, 1947 – died February 2, 1958)
Isaac Ghattas (June 21, 1949 – May 8, 1967), later Archbishop-Bishop of Minya of the Copts (Egypt) (May 8, 1967 – died June 8, 1977)
Amba Andraos Ghattas, Lazarists (C.M.) (May 8, 1967 – June 9, 1986), also Apostolic Administrator of Alexandria of the Copts (Egypt) (February 24, 1984 – June 9, 1986), President of Synod of the Catholic Coptic Church (1985 – March 30, 2006), President of Assembly of the Catholic Hierarchy of Egypt (1985 – March 30, 2006), later Coptic Catholic Patriarch of Alexandria (June 23, 1986 – retired March 30, 2006), created Cardinal-Patriarch (February 21, 2001 – died January 20, 2009), also President of Council of Catholic Patriarchs of the East (2003–2006)
Aghnatios Elias Yaacoub, Jesuits (S.J.) (July 15, 1986 – died March 12, 1994), previously Coadjutor Eparch of Assiut of the Copts (Egypt) (May 19, 1983 – July 15, 1986)
Youhannes Ezzat Zakaria Badir (June 24, 1994 – December 27, 2015), previously Eparch (Bishop) of Ismayliah of the Copts (Egypt) (November 23, 1992 – June 23, 1994)
Emmanuel (Khaled Ayad) Bishay (April 16, 2016 -
Economy
The economy of Luxor, like that of many other Egyptian cities, is heavily dependent on tourism. Since 1988, Luxor is the only city that offers hot air balloon rides in Egypt, which is a common activity for tourists. Large numbers of people also work in agriculture, particularly sugarcane. There are also many industries, such as the pottery industry used in eating and many other uses.
The local economy was hit by the Luxor massacre in 1997, in which a total of 64 people (including 59 visiting tourists) were killed, at the time the worst terrorist attack in Egypt (before the Sharm el-Sheikh terrorist attacks). The massacre reduced tourist numbers for several years. Following the 2011 Arab Spring, tourism to Egypt dropped significantly, again affecting local tourist markets. Nineteen Asian and European tourists died when a hot air balloon crashed early on Tuesday, February 26, 2013 near Luxor following a mid-air gas explosion. It was one of the worst accidents involving tourists in Egypt. The casualties included French, British, Hungarian, Japanese nationals and nine tourists from Hong Kong.
To make up for shortfalls of income, many cultivate their own food. Goat's cheese, pigeons, subsidized and home-baked bread and homegrown tomatoes are commonplace among the majority of its residents.
Tourism development
A controversial tourism development plan aims to transform Luxor into the biggest vast open-air museum. The master plan envisions new roads, five-star hotels, glitzy shops, and an IMAX theatre. The main attraction is an 11 million dollar project to unearth and restore the 2.7 kilometres (1.7 miles) long Avenue of Sphinxes that once linked Luxor and Karnak temples. The ancient processional road was built by the pharaoh Amenhotep III and took its final form under Nectanebo I in 400 BCE. Over a thousand sphinx statues lined the road now being excavated which was covered by silt, homes, mosques and churches. Excavation started around 2004.
On 18 April 2019, the Egyptian Government announced the discovery of a previously unopened coffin in Luxor, dated back to 18th dynasty of Upper and Lower Egypt. According to the Minister of Antiquities Khaled al-Anani, it is the biggest rock-cut tomb to be unearthed in the ancient city of Thebes. It is one of the largest, well-preserved tombs ever found near the ancient city of Luxor. On 24 November 2018, this discovery was preceded by the finding of a well-preserved mummy of a woman inside a previously unopened coffin dating back more than 3,000 years.
Infrastructure
A bridge was opened in 1998, a few kilometres upstream of the main town of Luxor, allowing ready land access from the east bank to the west bank. Traditionally river crossings have been the domain of several ferry services. The so-called 'local ferry' (also known as the 'National Ferry') continues to operate from a landing opposite the Temple of Luxor.
Transport to sites on the west bank are serviced by taxi drivers who often approach ferry passengers.[citation needed] There are also local cars that reach some of the monuments for 2 L.E., although tourists rarely use them. Alternatively, motorboats line both banks of the Nile all day providing a quicker, but more expensive (50 L.E.), crossing to the other side.
The city of Luxor on the east bank has several bus routes used mainly by locals. Tourists often rely on horse carriages, called "calèches", for transport or tours around the city. Taxis are plentiful, and reasonably priced, and since the government has decreed that taxis older than 20 years will not be relicensed, there are many modern air-conditioned cabs. Recently, new roads have been built in the city to cope with the growth in traffic.
For domestic travel along the route of the Nile, a rail service operates several times a day. A morning train and sleeping train can be taken from the railway station situated around 400 metres (440 yd) from Luxor Temple. The line runs between several major destinations, including Cairo to the north and Aswan to the south.
Luxor University
Luxor University, founded in 2019, is a non-profit governmental university that provides programs and courses for students.
Twin towns – sister cities
United States Baltimore, United States
Brazil Brasília, Brazil
Georgia (country) Kakheti, Georgia
Bulgaria Kazanlak, Bulgaria
China Shenzhen, China
Italy Viterbo, Italy
China Yangzhou, China
Lake Montezuma is a census-designated place (CDP) in Yavapai County in the U.S. state of Arizona. The population was 3,344 at the 2000 census. The CDP includes the communities of Rimrock and McGuireville. Located along Interstate 17, it is 20 miles (32 km) south of Sedona and 8 miles (13 km) north of Camp Verde in central Arizona's Verde Valley.
The community was originally known as Beaver Creek as ranchers and farmers settled along the banks of the creek named for the prolific numbers of beavers found there. In 1882, when there were a total of 8 local children, Yavapai County set up one of the first schools in the Verde Valley, Beaver Creek School, drawing kids from many miles around the area.
The area of the community known as McGuireville started in 1910 when Eugene McGuire settled near the confluence of Dry Beaver Creek and Wet Beaver Creek. This was also at the junction of the historic road from Stoneman Lake which split there with one route going on to Cornville, Cottonwood and Jerome and the other going south to Camp Verde and on to Prescott via Cherry. This later became the site of the first local business besides ranching and dudes when Midge Montgomery set up the original Beaver Creek Store there in 1931.
The area generally became known as Rimrock in 1926 when Virginia Finnie, the daughter of a prominent local rancher, started a dude ranch which she appropriately named Rimrock Guest Ranch. It was so named for the prominent limestone rimrocks forming the edges of the mesas visible from the hill top ranch.
Around 1957 shortly after the Black Canyon Highway was built north from Phoenix one of the largest ranches in Rimrock was turned into a subdivision called Lake Montezuma. The developers were planning on selling much of the property to out of state buyers and realized they needed something attractive in the name. They dug out a pond below the original ranch house and named it Lake Montezuma after the area's most significant local landmark - Montezuma Well National Monument.
The majority of the population of the rapidly growing area soon lived in this one subdivision and virtually all of them were not from the local area. They would identify themselves as being from Lake Montezuma not realizing that they might also be considered a resident of Rimrock and also Beaver Creek. Thus the confusion over the name of the general area.
en.wikipedia.org/wiki/Lake_Montezuma,_Arizona
en.wikipedia.org/wiki/Wikipedia:Text_of_Creative_Commons_...
A cold, frosty start to the day, but no evidence of snow in Shoreham. A bit sketchy for the ride to work - on the road, path and across the wooden deck of the Old Tollbridge.
The Four Bear Trailhead provides access to the Four Bear Trail that is suitable for horseback riding, hiking, and limited mountain biking. Facilities at the trailhead include an information kiosk, horse trailer parking, horse hitching rails, and toilet facilities. The trail provides access to Four Bear Mountain climbing north approximately four miles to the Shoshone National Forest boundary where it connects to many trails on the forest.
The Four Bear Trail also intersects the Jim Mountain Trail about two miles east of the U.S. Forest Service Jim Mountain Trailhead. The elevation ranges from 5,600 feet to 7,600 feet.
Spectacular views are offered of the North Fork Shoshone River valley and fascinating volcanic spires, turrets and banded rock formations. Wildlife such as deer, elk, grizzly and black bear, and numerous bird species such as golden eagles and mountain bluebirds are often found in the trail area. This is grizzly bear country, so be bear aware!
Photo by Rick Tryder.
DIRECTIONS
The trailhead is located 17 miles west of Cody on Wyoming State Highway 14-16-20 (the road to Yellowstone). Turn right at the Four Bear Trailhead sign.
LATITUDE/LONGITUDE
44.47578373 / -109.414787
PHONE 307-578-5900
EMAIL cody_wymail@blm.gov
ADDRESS Cody Field Office
1002 Blackburn St.
Cody, WY 82414
As part of Shared Streets, DOT Art in collaboration with the Mayor’s Office of Records present nine Art Display Structures that feature a variety of historical photographs and information about Lower Manhattan. The vinyl artwork includes events like the Broadway Canyon of Heroes Parade, the Wall Street Bombings as well as architectural drawings of the Brooklyn Bridge, South Street Seaport and ferry boats. Locations include: Spruce Street and Park Row, Fulton Street between Gold Street and Cliff Street, Fulton Street and Water Street and State Street and Broadway. In a few locations, cases are installed feet away from the event they are describing. For example, the South Street Seaport display case features information and renderings of the RMS Titanic Lighthouse that stands nearly 100 feet away from the case itself. The exhibition was presented in concurrence with Shared Streets, a new public spaces initiative that invites pedestrians and cyclists to share the streets of Lower Manhattan with vehicles traveling at 5 mph. Participants of the event held on August 13, 2016 were able to enjoy the Mayor’s Office of Records retrospective as they traveled the route.
NYCDOT Art Program, Art Display Case
Presented with the Mayor’s Office of Records
Spruce Street and Park Row, Fulton Street between Gold Street and Cliff Street, Fulton Street and Water Street and State Street and Broadway, Manhattan
Includes minifigures: 2 Aqua Scavengers, a dead underwater robber
Accessories include crowbar, laser cutter and harpoon
At Pevensey Castle
Pevensey Castle: a Saxon Shore fort, Norman defences, a medieval enclosure castle, and later associated remains
The monument includes Anderita Saxon Shore fort, traces of later, Norman defences, an enclosure castle, a 16th century gun emplacement and World War II defences situated on a low spur of sand and clay which now lies around 2km north west of the present East Sussex coastline at Pevensey. During the Roman and medieval periods the spur formed a peninsula projecting into a tidal lagoon and marshland, but coastal deposition and land reclamation have gradually built up the ground around it so that it is now completely land-locked. The roughly oval, north east-south west aligned Roman fort is the earliest of the structures which make up the monument and has been dated to the first half of the fourth century AD. Covering almost 4ha, the fort survives in the form of substantial ruins and buried remains. It is enclosed by a massive defensive wall with a flint and sandstone rubble core faced by coursed greensand and ironstone blocks, interspersed with red tile bonding courses. The whole is up to 3.7m thick and survives to a height of up to 8.1m. The wall was originally topped by a wall walk and parapet. Part excavation in 1906-8 showed that the wall was constructed on footings of rammed chalk and flints underpinned by oak piles and held together by a framework of wooden beams. Investigation of the internal face indicated that this was stepped upwards from a wide base so as to provide extra strength and support. Despite these precautions, a landslip on the south eastern side of the fort has resulted in the destruction of a c.180m length of the perimeter walls and, although fragments of the fallen masonry do survive, most have been removed over the years. Smaller sections of wall have also collapsed along the north western and eastern stretches. The defensive strength provided by the perimeter wall was enhanced by irregularly-spaced, externally projecting semicircular bastions with diameters of around 5m. There were originally at least 15 of these, of which 10 survive today. The fort was entered from its south western, landward approach by way of the main gateway. In front of this a protective ditch 5.5m wide was dug, and, although this became infilled over the years, a 40m stretch located towards its south eastern end has been recut and exposed. The ditch would have been spanned originally by a wooden bridge, although this no longer survives. The main gateway takes the form of a rectangular gatehouse set back between two solid semicircular bastions 8m apart. The 2.7m wide, originally arched entrance is flanked by two oblong guardrooms and the whole gateway structure projects beyond the inner face of the perimeter wall into the fort and is thought to have been originally two or even three storeys high. On the eastern side of the fort is a more simply designed subsidiary gateway, originally a 3m wide archway entrance, giving access to part of the adjacent Roman harbour, now overlain by Pevensey village. The extant archway is a modern reconstruction of the Norman rebuilding of the original entrance. Traces of a wooden causeway which led from it into the fort have been found during partial excavation. Midway along the north western stretch of perimeter wall is a now ruined postern c.2m wide, approached by a curved passage set within the wall. Part excavation between 1906-1908 indicated that the internal buildings which housed the garrison of up to 1,000 men, along with their livestock and supplies, were constructed of timber infilled with wattle and daub. A c.1m sq timber-lined Roman well was found in the south western sector of the fort, at the bottom of which were the remains of the wooden bucket with rope still attached. The well was found to have been filled with rubbish in Roman times and the presence of the bones of cattle, sheep, red deer, wild boar, wild birds, domestic dogs and cats, along with sea shells, gives some indication of the diet and lifestyle of the fort's original inhabitants. Anderita is thought to have been abandoned by its garrison by the latter half of the 4th century AD, and although little is known of its subsequent history until the 11th century, the Anglo-Saxon Chronicle records a massacre of Britons by the invading Saxons at the fort in AD 491. The Bayeux Tapestry states that William the Conquerer landed at Pevensey in 1066, and the Norman army are believed to have made use of the Roman fort as one of their first armed camps. The defences at Pevensey and the surrounding land were granted to King William's half-brother Robert, Count of Mortain. The medieval defences then went through at least 300 years of development, culminating in the construction of a stone built enclosure castle within the largely intact walls of the earlier Roman fort. It is thought that the first Norman defences took the form of a wooden palisade surrounded by a bank and ditch, and a c.40m length of partially infilled ditch up to 9m wide which survives across the north eastern sector of the earlier fort may indicate their original extent. Limited excavations in 1993-94 showed that the ground surface in the south eastern sector of the fort, in the vicinity of the later stone-built keep, was artificially raised some time before 1200, suggesting that a motte may also have been constructed. The original Roman gateways were rebuilt and a new ditch dug in front of the south western gate. Most of the Norman defences and interior wooden buildings will now survive in buried form beneath the later medieval castle, although herringbone-pattern repairs to the Roman masonry, by then serving as the outer bailey of the medieval defences, also date from this time. Around 1100 the defences were strengthened and the accommodation improved by the addition of a masonry keep in the south eastern sector of the earlier fort. The subject of a complex history of alteration, collapse and repair, the keep utilises part of the earlier, Roman perimeter wall and bastions. It takes the form of a rectangular block measuring c.16.8m by c.9m internally, reinforced by apsidal projections on all sides. Now surviving in ruined form up to first floor level, the keep originally took the form of a tall tower with an entrance on the first floor. A rectangular building measuring 7.6m by 6m was later constructed in the south eastern angle between the keep and the Roman wall. At around 1200 work began on the construction of a smaller, stone-built inner bailey in the south eastern sector of the earlier fort. An L-shaped ditch around 20m wide was dug to define the new enclosure, and this retains water in its northern arm. The material excavated from the ditch and from the destruction of the earlier bank was spread over much of the outer bailey to a depth of up to 1.5m. The ditch was recut during extensive renovations carried out during the early 20th century. The first structure to be built in this phase was the gatehouse to the south west which has an arched entrance between twin, semicircular external towers, now ruined. The basement chambers beneath each tower have ashlar-faced walls and barrel-vaulted ceilings, the southern chamber being entered by way of a newel staircase, the northern by a trapdoor. Both were used to house prisoners. Many subsequent alterations included the replacement, during the 15th century, of the wooden bridge over the outer ditch by a stone causeway. The originally embattled curtain wall enclosing the inner bailey was built within the ditch and inner berm around 1250. This survives almost to its full original height and is faced with coursed Greensand ashlar. Three semicircular external towers provided flanking cover from the narrow embrasures which pierce their walls. Each has a narrow staircase to a basement, a branch staircase off it into the ditch and a room and garderobe, or latrine, at ground floor level. Upper rooms were entered by way of the wall walk and were heated by fireplaces. The basement of the northernmost tower has two rib-vaulted bays, the keeled ribs resting on stiff-leaf corbels. The interior castle buildings continued to be built mainly of wood and these will survive in buried form, although the stone foundations of a chapel were exposed during partial excavation of the northern sector of the inner bailey. Around 20m south east of the chapel is a large stone-lined well at least 15.5m deep, and near this is a pile of medieval stone missile-balls, a selection of those recovered from the ditch. These were thrown from trebuchets during the four sieges of the castle. William, Count of Mortain forfeited Pevensey after an unsuccessful rebellion against Henry I in 1101 and the castle, which remained in the royal gift until the later Middle Ages, passed into the hands of the de Aquila family. The most famous siege took place in 1264-65 when the supporters of Henry III, fleeing from their defeat by the Barons at Lewes, took refuge in the castle. In 1372 the castle was given to John of Gaunt, and during his period of office was used to imprison James I, King of Scotland, who had been seized in 1406, and Joan, Queen of Navarre, accused of witchcraft by her stepson, Henry V. By 1300, the sea had gradually begun to recede from around the castle and its military importance declined as a result. Contemporary records show that the castle walls were constantly in need of expensive repair and by the end of the 14th century were not being properly maintained, although the roof leads were kept intact until the middle of the 15th century. By 1500 the castle had ceased to be inhabited and fell rapidly into decay. The threat of the Spanish Armada led to some renewed interest in the defensive value of the site, and a survey of 1587 records that the castle housed two demi-culverins, or heavy guns. These were sited on the contemporary, south east orientated, M-shaped earthen gun emplacement situated in the outer bailey around 90m north east of the main Roman gateway. This takes the form of a raised level platform c.20m long bounded on the seaward side by a slight bank c.0.4m high and around 3m wide. One of the cast iron guns, manufactured in the East Sussex Weald, is now housed within the inner bailey on a modern replica carriage. From the 17th century the castle passed through the hands of various private owners. Valued as a picturesque ruin during the 18th and 19th centuries, it features in many contemporary engravings and illustrations. In 1925 the Duke of Devonshire presented the monument to the state, and extensive repairs began with a view to opening the monument to the public. These were interrupted by the outbreak of World War II, when the castle resumed its original military purpose of protecting the south coast. The castle was refortified in May 1940 as an observation and command post. It was continuously occupied by regular troops, including Canadian forces and the United States Army Air Corps, who used it as a radio direction centre, and by the Home Guard until 1944. The World War II defences include two pillboxes and three machine gun posts of concrete faced with rubble and flints, carefully concealed and camouflaged within the earlier Roman and medieval fabric. An internal tower was built just to the south of the Roman east gateway and a blockhouse housing anti-tank weapons was built in front of the main Roman gateway. The blockhouse no longer survives. Modifications carried out to the medieval mural towers included lining the interiors with brick and inserting wooden floors. In 1945 the monument was returned to peaceful use and is now in the guardianship of the Secretary of State and open to the public.
[Historic England]
The “INKredible 2″ Pack includes 20 NEW polymer clay patterns sheets designs introducing a variety & mix of materials to use along with alcohol inks.
These sheets can be applied in any bead, jewel, or accessory of your choice – flat or curved, small or large.
I implemented my pattern sheets on earrings & beads.
The materials I used are probably already in your polymer clay toolbox, taken from many of my previous classes –
Alcohol inks, chalk pastels, paints, stazon inks, stencils etc.
This class is a new version of my known previous INKredible class, now offering a celebration of exciting, new techniques, encouraging you to use anything on your worktable, along with alcohol inks.
20 patterns came out of my personal laboratory, but the combinations are infinite!
www.polypediaonlineexpress.com/product/complete-inkredibl...
If you are interested in combining these beads in elaborated, impressive Micro Macrame knotting, you are welcome to check out the new "INKredible Macrame" class -
www.polypediaonlineexpress.com/inkredible2-inkredible-mac...
This compilation video shows a chase of ARR 4006 as it leads a freight train south toward Seward. Filming locations include Rainbow, Bird Point, and Moose Pass, AK. As seen in the video, this train departed Anchorage well before sunrise which, at this time of year, didn't occur until ~1000L, so the first two locations were shot before the sun came up over the Chugach Mountains.
The tide in the Turnagain Arm, home of some of the largest boretides in the world, is on its way out. Photos and video along the Turnagain always turn out better when there's more water than not, so I was lucky to at least have some water present!
The final location in Moose Pass is, to me, a little slice of heaven. I just wish this location saw more than one or two trains per week in the winter time. If there were more trains, I'd probably camp out here for days at a time! As it is though, you have to take what you can get.
Also, Chris Laskowski, *this* is why you need to bring C. Vision Productions up here!
The Dallas Arts District's "Spotlight Sunday" on October 18
Festivities to celebrate the opening of the new AT&T Performing Arts Center include a day of free admission and extended hours. Enjoy performances in the exhibition All the World’s a Stage, tours family experiences, and much more.
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The Dallas Arts District
2200 Ross Ave
Dallas, TX 75201
(214) 744-6642
The Dallas Arts District is a unique, 68-acre, 19-block neighborhood in the heart of the city. A rare jewel that is the centerpiece of the region’s cultural life, the District is home to some of the finest architecture in the world. Enhancing the downtown Dallas skyline are buildings by Pritzker Prize winners I.M. Pei, Renzo Piano, Norman Foster, Rem Koolhaas and AIA “Gold Medal” recipient Edward Larrabee Barnes.
Our neighborhood is a center for innovative architecture, world-class exhibits, exemplary cultural programming and much more. We are restaurants, hotels, churches, residences and even the world headquarters of 7-Eleven.
This website is designed to help you explore the many facets of the district. And whether you are coming from around the corner or from around the world, we hope you will find your trip enjoyable and your experience unparalleled.
We look forward to sharing with you the works of art, the performances, the cuisine and the vibrancy of the Dallas Arts District.
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Dallas Museum of Art
The Dallas Museum of Art ranks among leading art institutions in the country and is distinguished by its innovative exhibitions and groundbreaking educational programs.
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Nasher Sculpture Center
The Nasher Sculpture Center opened in 2003 as the first institution in the world dedicated exclusively to the exhibition of modern and contemporary sculpture with a collection of global significance at its foundation.
www.nashersculpturecenter.org/
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Trammell Crow Center and Crow Collection of Asian Art
The Trammell and Margaret Crow Collection of Asian Art is nestled like a small jewel in Dallas’ Arts District, offering visitors a glimpse of a world possessing serene beauty and spirituality in the heart of a bustling city.
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Belo Mansion
The current home of the Dallas Bar Association, the Belo Mansion was built c. 1890 by Coleonel A. H. Belo, founder of the Dallas Morning News.
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Cathedral Shrine of the Virgin of Guadalupe
The city’s oldest Catholic parish, this High Victorian Gothic cathedral is the second busiest Catholic cathedral in the nation.
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Morton H. Meyerson Symphony Center
Since its grand opening celebration, the legendary rich sound of the Meyerson’s Eugene McDermott Concert Hall has made it a premier destination for the world’s finest soloists and conductors.
www.dallasculture.org/meyersonSymphonyCenter/
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AT&T Performing Arts Center Margot and Bill Winspear Opera House
With transparent, soaring 60-foot glass walls revealing views of the Grand Lobby and a café open throughout the day, the Winspear Opera House is a destination for all.
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AT&T Performing Arts Center Dee and Charles Wyly Theatre
The world’s only vertical theatre, the innovative design of the Wyly Theatre creates ultimate performance flexibility.
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Booker T. Washington High School for the Visual and Performing Arts
The school’s dual emphasis on arts and academics has produced a stellar list of famous graduates including Grammy Award®-winners Norah Jones, Erykah Badu and jazz trumpeter Roy Hargrove.
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St. Paul United Methodist Church
St. Paul United Methodist Church was founded in 1873 by freed slaves from Mississippi, Louisiana and Texas.
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One Arts Plaza
One Arts Plaza is a multiuse structure comprised of residences, corporate offices and retail, the first of three buildings on over 10 acres at the eastern edge of the Dallas Arts District.
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Dallas Black Dance Theatre
Dallas Black Dance Theatre is the city’s oldest continuously operating dance company.
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AT&T Performing Arts Center Elaine D. and Charles A. Sammons Park
Weaving together the Winspear Opera House, Wyly Theatre, Strauss Square and City Performance Hall, the ten-acre park stretches from Woodall Rodgers Freeway to Ross Avenue, and is the first public park in the Dallas Arts District.
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From the upper outside balcony of the AT&T Performing Arts Center Margot and Bill Winspear Opera House