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In Nature, I find peace and spiritual guidance…the forest is my temple…When you loose what you have you reinvent yourself!
The RAD project: (A roll in a day/a day in a roll) www.flickr.com/groups/rollinaday/
Snapshots of a 3-hour cruise aboard the historic ferry Proclaim on Sydney Harbour, visiting Fort Denison where we had morning tea, and Garden Island. The commentary was about what happened on the night of 31 May 1942, when four Japanese midget submarines entered Sydney Harbour.
The historic ferry Proclaim, built in 1939, just in front of the Opera House, approaching. We knew that this excursion was going to be on a historic ferry . So, prior to our excursion I googled to find out what a historic ferry may look like. I came across some unrenovated ferries and thought surely not. And then this delightful little ferry came scooting around the massive Explorers of the Sea. It was chartered just for our group. rosman.com.au/our-fleet/proclaim
FILMPROCESSING, PRINTING, SCANNING, C-41 <a www.facebook.com/Bennetts-Photos-Frames-formerly-Just-Pho... Bennett's Photos & Frames, Mortdale, NSW Australia
Santa Maria in Campitelli or Santa Maria in Portico is a church dedicated to the Virgin Mary on the Piazza di Campitelli, Rome, Italy.
The church contains a 25 cm-high icon of the Virgin Mary dated by style and dendrochronology to the 11th century, though it had previously been claimed by tradition to have appeared miraculously in 524 at the table of Galla, a Roman woman who was helping the poor, and then carried in processions since 590. It was previously housed in the now-demolished Oratory of Santa Gala, sited at what is now the piazza's far end near the Porticus Octaviae (giving the church and icon its name of "Madonna of the Portico").
The icon was believed to have saved the city from plague in 1656 (or 1658), when it was carried in procession through the streets. On account of this, the earlier church on this site was replaced by Pope Alexander VII between 1659 and 1667 with the present one, designed by Carlo Rainaldi in the high Baroque style.
The present church has a travertine façade with large columns against (but not attached to) it, thus giving it strong vertical lines. The original design included statues which were however never executed.
Metro
Beijing, China
July 2012
Candid shots in and around Public Transport
Ricoh GRD IV
Please do not reproduce or use this picture without my explicit permission.
If you ask nicely I will probably say yes, just ask me first!
If you happen to be in one of my frames and have any objections to this.
Please contact me!
Please no glossy awards, scripted comments and big thumbnails back to your own work.
I will remove them...
In the American cities, the main church is located in the central square, but in the case of the San Gabriel village, it is located at a block of distance from the main plaza and reproducing what the Indian laws (Leyes de Indias) mentioned in the case of the main temple: "In Mediterranean places the temple is not build in the square, but somewhat distant from it, .... and that it can be seen of all parts and better venerated.
This is the only church in Ecuador that has been build that way.
Thanks for taking the time to comment, I really appreciate it and
will always try to reciprocate with a visit back to your stream.
© Henri Leduc - All of my images are protected by copyright
Some of my images are for sale via Getty Images and 500px
After saying before in the description of the charity bus repaint that I didn't want to tackle 603's vinyl wrap - guess what I then went and did..?
I had a moment like the boys from (proper) Top Gear and questioned "how hard can it be?"
Well, after several days at it, I finally believe I have finished it to a decent enough level to be called done. True, it isn't 100% accurate to the real bus but I'd go as far as to say it's quite close. And as to how hard it was, well let's just say it was getting tedious by the end and an enormous relief when I discovered the stick figures on the nearside were pretty much all duplicates of ones on the offside - meaning I had much less work to do on the nearside than I first thought!
Livery available to be downloaded from:
fellowsfilm.com/downloads/nottingham-city-transport-c400r...
Canyonlands National Park is an American national park located in southeastern Utah near the town of Moab. The park preserves a colorful landscape eroded into numerous canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964.
The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the combined rivers—the Green and Colorado—which carved two large canyons into the Colorado Plateau. While these areas share a primitive desert atmosphere, each retains its own character. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
In the early 1950s, Bates Wilson, then superintendent of Arches National Monument, began exploring the area to the south and west of Moab, Utah. After seeing what is now known as the Needles District of Canyonlands National Park, Wilson began advocating for the establishment of a new national park that would include the Needles. Additional explorations by Wilson and others expanded the areas proposed for inclusion into the new national park to include the confluence of Green and Colorado rivers, the Maze District, and Horseshoe Canyon.
In 1961, Secretary of the Interior Stewart Udall was scheduled to address a conference at Grand Canyon National Park. On his flight to the conference, he flew over the Confluence (where the Colorado and Green rivers meet). The view apparently sparked Udall's interest in Wilson's proposal for a new national park in that area and Udall began promoting the establishment of Canyonlands National Park.
Utah Senator Frank Moss first introduced legislation into Congress to create Canyonlands National Park. His legislation attempted to satisfy both nature preservationists' and commercial developers' interests. Over the next four years, his proposal was struck down, debated, revised, and reintroduced to Congress many times before being passed and signed into creation.
In September, 1964, after several years of debate, President Lyndon B. Johnson signed Pub.L. 88–590, which established Canyonlands National Park as a new national park. Bates Wilson became the first superintendent of the new park and is often referred to as the "Father of Canyonlands."
The Colorado River and Green River combine within the park, dividing it into three districts called the Island in the Sky, the Needles, and the Maze. The Colorado River flows through Cataract Canyon below its confluence with the Green River.
The Island in the Sky district is a broad and level mesa in the northern section of the park, between the Colorado and Green rivers. The district has many viewpoints overlooking the White Rim, a sandstone bench 1,200 feet (370 m) below the Island, and the rivers, which are another 1,000 feet (300 m) below the White Rim.
The Needles district is located south of the Island in the Sky, on the east side of the Colorado River. The district is named for the red and white banded rock pinnacles which are a major feature of the area. Various other naturally sculpted rock formations are also within this district, including grabens, potholes, and arches. Unlike Arches National Park, where many arches are accessible by short to moderate hikes, most of the arches in the Needles district lie in backcountry canyons, requiring long hikes or four-wheel drive trips to reach them.
The Ancestral Puebloans inhabited this area and some of their stone and mud dwellings are well-preserved, although the items and tools they used were mostly removed by looters. The Ancestral Puebloans also created rock art in the form of petroglyphs, most notably on Newspaper Rock along the Needles access road.
The Maze district is located west of the Colorado and Green rivers. The Maze is the least accessible section of the park, and one of the most remote and inaccessible areas of the United States.
A geographically detached section of the park located north of the Maze district, Horseshoe Canyon contains panels of rock art made by hunter-gatherers from the Late Archaic Period (2000-1000 BC) pre-dating the Ancestral Puebloans. Originally called Barrier Canyon, Horseshoe's artifacts, dwellings, pictographs, and murals are some of the oldest in America. The images depicting horses date from after 1540 AD, when the Spanish reintroduced horses to America.
Since the 1950s, scientists have been studying an area of 200 acres (81 ha) completely surrounded by cliffs. The cliffs have prevented cattle from ever grazing on the area's 62 acres (25 ha) of grassland. According to the scientists, the site may contain the largest undisturbed grassland in the Four Corners region. Studies have continued biannually since the mid-1990s. The area has been closed to the public since 1993 to maintain the nearly pristine environment.
Mammals that roam this park include black bears, coyotes, skunks, bats, elk, foxes, bobcats, badgers, ring-tailed cats, pronghorns, desert bighorn sheep, and cougars. Desert cottontails, kangaroo rats and mule deer are commonly seen by visitors.
At least 273 species of birds inhabit the park. A variety of hawks and eagles are found, including the Cooper's hawk, the northern goshawk, the sharp-shinned hawk, the red-tailed hawk, the golden and bald eagles, the rough-legged hawk, the Swainson's hawk, and the northern harrier. Several species of owls are found, including the great horned owl, the northern saw-whet owl, the western screech owl, and the Mexican spotted owl. Grebes, woodpeckers, ravens, herons, flycatchers, crows, bluebirds, wrens, warblers, blackbirds, orioles, goldfinches, swallows, sparrows, ducks, quail, grouse, pheasants, hummingbirds, falcons, gulls, and ospreys are some of the other birds that can be found.
Several reptiles can be found, including eleven species of lizards and eight species of snake (including the midget faded rattlesnake). The common kingsnake and prairie rattlesnake have been reported in the park, but not confirmed by the National Park Service.
The park is home to six confirmed amphibian species, including the red-spotted toad, Woodhouse's toad, American bullfrog, northern leopard frog, Great Basin spadefoot toad, and tiger salamander. The canyon tree frog was reported to be in the park in 2000, but was not confirmed during a study in 2004.
Canyonlands National Park contains a wide variety of plant life, including 11 cactus species,[34] 20 moss species, liverworts, grasses and wildflowers. Varieties of trees include netleaf hackberry, Russian olive, Utah juniper, pinyon pine, tamarisk, and Fremont's cottonwood. Shrubs include Mormon tea, blackbrush, four-wing saltbush, cliffrose, littleleaf mountain mahogany, and snakeweed
Cryptobiotic soil is the foundation of life in Canyonlands, providing nitrogen fixation and moisture for plant seeds. One footprint can destroy decades of growth.
According to the Köppen climate classification system, Canyonlands National Park has a cold semi-arid climate ("BSk"). The plant hardiness zones at the Island in the Sky and Needles District Visitor Centers are 7a with an average annual extreme minimum air temperature of 4.0 °F (-15.6 °C) and 2.9 °F (-16.2 °C), respectively.
The National Weather Service has maintained two cooperative weather stations in the park since June 1965. Official data documents the desert climate with less than 10 inches (250 millimetres) of annual rainfall, as well as hot, mostly dry summers and cold, occasionally wet winters. Snowfall is generally light during the winter.
The station in The Neck region reports an average January temperature of 29.6 °F and an average July temperature of 79.3 °F. Average July temperatures range from a high of 90.8 °F (32.7 °C) to a low of 67.9 °F (19.9 °C). There are an average of 45.7 days with highs of 90 °F (32 °C) or higher and an average of 117.3 days with lows of 32 °F (0 °C) or lower. The highest recorded temperature was 105 °F (41 °C) on July 15, 2005, and the lowest recorded temperature was −13 °F (−25 °C) on February 6, 1989. Average annual precipitation is 9.33 inches (237 mm). There are an average of 59 days with measurable precipitation. The wettest year was 1984, with 13.66 in (347 mm), and the driest year was 1989, with 4.63 in (118 mm). The most precipitation in one month was 5.19 in (132 mm) in October 2006. The most precipitation in 24 hours was 1.76 in (45 mm) on April 9, 1978. Average annual snowfall is 22.8 in (58 cm). The most snowfall in one year was 47.4 in (120 cm) in 1975, and the most snowfall in one month was 27.0 in (69 cm) in January 1978.
The station in The Needles region reports an average January temperature of 29.7 °F and an average July temperature of 79.1 °F.[44] Average July temperatures range from a high of 95.4 °F (35.2 °C) to a low of 62.4 °F (16.9 °C). There are an average of 75.4 days with highs of 90 °F (32 °C) or higher and an average of 143.6 days with lows of 32 °F (0 °C) or lower. The highest recorded temperature was 107 °F (42 °C) on July 13, 1971, and the lowest recorded temperature was −16 °F (−27 °C) on January 16, 1971. Average annual precipitation is 8.49 in (216 mm). There are an average of 56 days with measurable precipitation. The wettest year was 1969, with 11.19 in (284 mm), and the driest year was 1989, with 4.25 in (108 mm). The most precipitation in one month was 4.43 in (113 mm) in October 1972. The most precipitation in 24 hours was 1.56 in (40 mm) on September 17, 1999. Average annual snowfall is 14.4 in (37 cm). The most snowfall in one year was 39.3 in (100 cm) in 1975, and the most snowfall in one month was 24.0 in (61 cm) in March 1985.
National parks in the Western US are more affected by climate change than the country as a whole, and the National Park Service has begun research into how exactly this will effect the ecosystem of Canyonlands National Park and the surrounding areas and ways to protect the park for the future. The mean annual temperature of Canyonlands National Park increased by 2.6 °F (1.4 °C) from 1916 to 2018. It is predicted that if current warming trends continue, the average highs in the park during the summer will be over 100 °F (40 °C) by 2100. In addition to warming, the region has begun to see more severe and frequent droughts which causes native grass cover to decrease and a lower flow of the Colorado River. The flows of the Upper Colorado Basin have decreased by 300,000 acre⋅ft (370,000,000 m3) per year, which has led to a decreased amount of sediment carried by the river and rockier rapids which are more frequently impassable to rafters. The area has also begun to see an earlier spring, which will lead to changes in the timing of leaves and flowers blooming and migrational patterns of wildlife that could lead to food shortages for the wildlife, as well as a longer fire season.
The National Park Service is currently closely monitoring the impacts of climate change in Canyonlands National Park in order to create management strategies that will best help conserve the park's landscapes and ecosystems for the long term. Although the National Park Service's original goal was to preserve landscapes as they were before European colonization, they have now switched to a more adaptive management strategy with the ultimate goal of conserving the biodiversity of the park. The NPS is collaborating with other organizations including the US Geological Survey, local indigenous tribes, and nearby universities in order to create a management plan for the national park. Right now, there is a focus on research into which native plants will be most resistant to climate change so that the park can decide on what to prioritize in conservation efforts. The Canyonlands Natural History Association has been giving money to the US Geological Survey to fund this and other climate related research. They gave $30,000 in 2019 and $61,000 in 2020.
A subsiding basin and nearby uplifting mountain range (the Uncompahgre) existed in the area in Pennsylvanian time. Seawater trapped in the subsiding basin created thick evaporite deposits by Mid Pennsylvanian. This, along with eroded material from the nearby mountain range, became the Paradox Formation, itself a part of the Hermosa Group. Paradox salt beds started to flow later in the Pennsylvanian and probably continued to move until the end of the Jurassic. Some scientists believe Upheaval Dome was created from Paradox salt bed movement, creating a salt dome, but more modern studies show that the meteorite theory is more likely to be correct.
A warm shallow sea again flooded the region near the end of the Pennsylvanian. Fossil-rich limestones, sandstones, and shales of the gray-colored Honaker Trail Formation resulted. A period of erosion then ensued, creating a break in the geologic record called an unconformity. Early in the Permian an advancing sea laid down the Halgaito Shale. Coastal lowlands later returned to the area, forming the Elephant Canyon Formation.
Large alluvial fans filled the basin where it met the Uncompahgre Mountains, creating the Cutler red beds of iron-rich arkose sandstone. Underwater sand bars and sand dunes on the coast inter-fingered with the red beds and later became the white-colored cliff-forming Cedar Mesa Sandstone. Brightly colored oxidized muds were then deposited, forming the Organ Rock Shale. Coastal sand dunes and marine sand bars once again became dominant, creating the White Rim Sandstone.
A second unconformity was created after the Permian sea retreated. Flood plains on an expansive lowland covered the eroded surface and mud built up in tidal flats, creating the Moenkopi Formation. Erosion returned, forming a third unconformity. The Chinle Formation was then laid down on top of this eroded surface.
Increasingly dry climates dominated the Triassic. Therefore, sand in the form of sand dunes invaded and became the Wingate Sandstone. For a time climatic conditions became wetter and streams cut channels through the sand dunes, forming the Kayenta Formation. Arid conditions returned to the region with a vengeance; a large desert spread over much of western North America and later became the Navajo Sandstone. A fourth unconformity was created by a period of erosion.
Mud flats returned, forming the Carmel Formation, and the Entrada Sandstone was laid down next. A long period of erosion stripped away most of the San Rafael Group in the area, along with any formations that may have been laid down in the Cretaceous period.
The Laramide orogeny started to uplift the Rocky Mountains 70 million years ago and with it, the Canyonlands region. Erosion intensified and when the Colorado River Canyon reached the salt beds of the Paradox Formation the overlying strata extended toward the river canyon, forming features such as The Grabens. Increased precipitation during the ice ages of the Pleistocene quickened the rate of canyon excavation along with other erosion. Similar types of erosion are ongoing, but occur at a slower rate.
Utah is a landlocked state in the Mountain West subregion of the Western United States. It borders Colorado to its east, Wyoming to its northeast, Idaho to its north, Arizona to its south, and Nevada to its west. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.
Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo, and Ute. The Spanish were the first Europeans to arrive in the mid-16th century, though the region's difficult geography and harsh climate made it a peripheral part of New Spain and later Mexico. Even while it was Mexican territory, many of Utah's earliest settlers were American, particularly Mormons fleeing marginalization and persecution from the United States via the Mormon Trail. Following the Mexican–American War in 1848, the region was annexed by the U.S., becoming part of the Utah Territory, which included what is now Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah's admission as a state; only after the outlawing of polygamy was it admitted in 1896 as the 45th.
People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. A 2023 paper challenged this perception (claiming only 42% of Utahns are Mormons) however most statistics still show a majority of Utah residents belong to the LDS church; estimates from the LDS church suggests 60.68% of Utah's population belongs to the church whilst some sources put the number as high as 68%. The paper replied that membership count done by the LDS Church is too high for several reasons. The LDS Church greatly influences Utahn culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.
Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. Utah ranks among the overall best states in metrics such as healthcare, governance, education, and infrastructure. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah's water security and impacting the state's economy.
The History of Utah is an examination of the human history and social activity within the state of Utah located in the western United States.
Archaeological evidence dates the earliest habitation of humans in Utah to about 10,000 to 12,000 years ago. Paleolithic people lived near the Great Basin's swamps and marshes, which had an abundance of fish, birds, and small game animals. Big game, including bison, mammoths and ground sloths, also were attracted to these water sources. Over the centuries, the mega-fauna died, this population was replaced by the Desert Archaic people, who sheltered in caves near the Great Salt Lake. Relying more on gathering than the previous Utah residents, their diet was mainly composed of cattails and other salt tolerant plants such as pickleweed, burro weed and sedge. Red meat appears to have been more of a luxury, although these people used nets and the atlatl to hunt water fowl, ducks, small animals and antelope. Artifacts include nets woven with plant fibers and rabbit skin, woven sandals, gaming sticks, and animal figures made from split-twigs. About 3,500 years ago, lake levels rose and the population of Desert Archaic people appears to have dramatically decreased. The Great Basin may have been almost unoccupied for 1,000 years.
The Fremont culture, named from sites near the Fremont River in Utah, lived in what is now north and western Utah and parts of Nevada, Idaho and Colorado from approximately 600 to 1300 AD. These people lived in areas close to water sources that had been previously occupied by the Desert Archaic people, and may have had some relationship with them. However, their use of new technologies define them as a distinct people. Fremont technologies include:
use of the bow and arrow while hunting,
building pithouse shelters,
growing maize and probably beans and squash,
building above ground granaries of adobe or stone,
creating and decorating low-fired pottery ware,
producing art, including jewelry and rock art such as petroglyphs and pictographs.
The ancient Puebloan culture, also known as the Anasazi, occupied territory adjacent to the Fremont. The ancestral Puebloan culture centered on the present-day Four Corners area of the Southwest United States, including the San Juan River region of Utah. Archaeologists debate when this distinct culture emerged, but cultural development seems to date from about the common era, about 500 years before the Fremont appeared. It is generally accepted that the cultural peak of these people was around the 1200 CE. Ancient Puebloan culture is known for well constructed pithouses and more elaborate adobe and masonry dwellings. They were excellent craftsmen, producing turquoise jewelry and fine pottery. The Puebloan culture was based on agriculture, and the people created and cultivated fields of maize, beans, and squash and domesticated turkeys. They designed and produced elaborate field terracing and irrigation systems. They also built structures, some known as kivas, apparently designed solely for cultural and religious rituals.
These two later cultures were roughly contemporaneous, and appear to have established trading relationships. They also shared enough cultural traits that archaeologists believe the cultures may have common roots in the early American Southwest. However, each remained culturally distinct throughout most of their existence. These two well established cultures appear to have been severely impacted by climatic change and perhaps by the incursion of new people in about 1200 CE. Over the next two centuries, the Fremont and ancient Pueblo people may have moved into the American southwest, finding new homes and farmlands in the river drainages of Arizona, New Mexico and northern Mexico.
In about 1200, Shoshonean speaking peoples entered Utah territory from the west. They may have originated in southern California and moved into the desert environment due to population pressure along the coast. They were an upland people with a hunting and gathering lifestyle utilizing roots and seeds, including the pinyon nut. They were also skillful fishermen, created pottery and raised some crops. When they first arrived in Utah, they lived as small family groups with little tribal organization. Four main Shoshonean peoples inhabited Utah country. The Shoshone in the north and northeast, the Gosiutes in the northwest, the Utes in the central and eastern parts of the region and the Southern Paiutes in the southwest. Initially, there seems to have been very little conflict between these groups.
In the early 16th century, the San Juan River basin in Utah's southeast also saw a new people, the Díne or Navajo, part of a greater group of plains Athabaskan speakers moved into the Southwest from the Great Plains. In addition to the Navajo, this language group contained people that were later known as Apaches, including the Lipan, Jicarilla, and Mescalero Apaches.
Athabaskans were a hunting people who initially followed the bison, and were identified in 16th-century Spanish accounts as "dog nomads". The Athabaskans expanded their range throughout the 17th century, occupying areas the Pueblo peoples had abandoned during prior centuries. The Spanish first specifically mention the "Apachu de Nabajo" (Navaho) in the 1620s, referring to the people in the Chama valley region east of the San Juan River, and north west of Santa Fe. By the 1640s, the term Navaho was applied to these same people. Although the Navajo newcomers established a generally peaceful trading and cultural exchange with the some modern Pueblo peoples to the south, they experienced intermittent warfare with the Shoshonean peoples, particularly the Utes in eastern Utah and western Colorado.
At the time of European expansion, beginning with Spanish explorers traveling from Mexico, five distinct native peoples occupied territory within the Utah area: the Northern Shoshone, the Goshute, the Ute, the Paiute and the Navajo.
The Spanish explorer Francisco Vázquez de Coronado may have crossed into what is now southern Utah in 1540, when he was seeking the legendary Cíbola.
A group led by two Spanish Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the California coast. The expedition traveled as far north as Utah Lake and encountered the native residents. All of what is now Utah was claimed by the Spanish Empire from the 1500s to 1821 as part of New Spain (later as the province Alta California); and subsequently claimed by Mexico from 1821 to 1848. However, Spain and Mexico had little permanent presence in, or control of, the region.
Fur trappers (also known as mountain men) including Jim Bridger, explored some regions of Utah in the early 19th century. The city of Provo was named for one such man, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah is named for a brigade leader of the Hudson's Bay Company, Peter Skene Ogden who trapped in the Weber Valley. In 1846, a year before the arrival of members from the Church of Jesus Christ of latter-day Saints, the ill-fated Donner Party crossed through the Salt Lake valley late in the season, deciding not to stay the winter there but to continue forward to California, and beyond.
Members of the Church of Jesus Christ of Latter-day Saints, commonly known as Mormon pioneers, first came to the Salt Lake Valley on July 24, 1847. At the time, the U.S. had already captured the Mexican territories of Alta California and New Mexico in the Mexican–American War and planned to keep them, but those territories, including the future state of Utah, officially became United States territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 10, 1848.
Upon arrival in the Salt Lake Valley, the Mormon pioneers found no permanent settlement of Indians. Other areas along the Wasatch Range were occupied at the time of settlement by the Northwestern Shoshone and adjacent areas by other bands of Shoshone such as the Gosiute. The Northwestern Shoshone lived in the valleys on the eastern shore of Great Salt Lake and in adjacent mountain valleys. Some years after arriving in the Salt Lake Valley Mormons, who went on to colonize many other areas of what is now Utah, were petitioned by Indians for recompense for land taken. The response of Heber C. Kimball, first counselor to Brigham Young, was that the land belonged to "our Father in Heaven and we expect to plow and plant it." A 1945 Supreme Court decision found that the land had been treated by the United States as public domain; no aboriginal title by the Northwestern Shoshone had been recognized by the United States or extinguished by treaty with the United States.
Upon arriving in the Salt Lake Valley, the Mormons had to make a place to live. They created irrigation systems, laid out farms, built houses, churches, and schools. Access to water was crucially important. Almost immediately, Brigham Young set out to identify and claim additional community sites. While it was difficult to find large areas in the Great Basin where water sources were dependable and growing seasons long enough to raise vitally important subsistence crops, satellite communities began to be formed.
Shortly after the first company arrived in the Salt Lake Valley in 1847, the community of Bountiful was settled to the north. In 1848, settlers moved into lands purchased from trapper Miles Goodyear in present-day Ogden. In 1849, Tooele and Provo were founded. Also that year, at the invitation of Ute chief Wakara, settlers moved into the Sanpete Valley in central Utah to establish the community of Manti. Fillmore, Utah, intended to be the capital of the new territory, was established in 1851. In 1855, missionary efforts aimed at western native cultures led to outposts in Fort Lemhi, Idaho, Las Vegas, Nevada and Elk Mountain in east-central Utah.
The experiences of returning members of the Mormon Battalion were also important in establishing new communities. On their journey west, the Mormon soldiers had identified dependable rivers and fertile river valleys in Colorado, Arizona and southern California. In addition, as the men traveled to rejoin their families in the Salt Lake Valley, they moved through southern Nevada and the eastern segments of southern Utah. Jefferson Hunt, a senior Mormon officer of the Battalion, actively searched for settlement sites, minerals, and other resources. His report encouraged 1851 settlement efforts in Iron County, near present-day Cedar City. These southern explorations eventually led to Mormon settlements in St. George, Utah, Las Vegas and San Bernardino, California, as well as communities in southern Arizona.
Prior to establishment of the Oregon and California trails and Mormon settlement, Indians native to the Salt Lake Valley and adjacent areas lived by hunting buffalo and other game, but also gathered grass seed from the bountiful grass of the area as well as roots such as those of the Indian Camas. By the time of settlement, indeed before 1840, the buffalo were gone from the valley, but hunting by settlers and grazing of cattle severely impacted the Indians in the area, and as settlement expanded into nearby river valleys and oases, indigenous tribes experienced increasing difficulty in gathering sufficient food. Brigham Young's counsel was to feed the hungry tribes, and that was done, but it was often not enough. These tensions formed the background to the Bear River massacre committed by California Militia stationed in Salt Lake City during the Civil War. The site of the massacre is just inside Preston, Idaho, but was generally thought to be within Utah at the time.
Statehood was petitioned for in 1849-50 using the name Deseret. The proposed State of Deseret would have been quite large, encompassing all of what is now Utah, and portions of Colorado, Idaho, Nevada, Wyoming, Arizona, Oregon, New Mexico and California. The name of Deseret was favored by the LDS leader Brigham Young as a symbol of industry and was derived from a reference in the Book of Mormon. The petition was rejected by Congress and Utah did not become a state until 1896, following the Utah Constitutional Convention of 1895.
In 1850, the Utah Territory was created with the Compromise of 1850, and Fillmore (named after President Fillmore) was designated the capital. In 1856, Salt Lake City replaced Fillmore as the territorial capital.
The first group of pioneers brought African slaves with them, making Utah the only place in the western United States to have African slavery. Three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with this first group in 1847. The settlers also began to purchase Indian slaves in the well-established Indian slave trade, as well as enslaving Indian prisoners of war. In 1850, 26 slaves were counted in Salt Lake County. Slavery didn't become officially recognized until 1852, when the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners were passed. Slavery was repealed on June 19, 1862, when Congress prohibited slavery in all US territories.
Disputes between the Mormon inhabitants and the federal government intensified after the Church of Jesus Christ of Latter-day Saints' practice of polygamy became known. The polygamous practices of the Mormons, which were made public in 1854, would be one of the major reasons Utah was denied statehood until almost 50 years after the Mormons had entered the area.
After news of their polygamous practices spread, the members of the LDS Church were quickly viewed by some as un-American and rebellious. In 1857, after news of a possible rebellion spread, President James Buchanan sent troops on the Utah expedition to quell the growing unrest and to replace Brigham Young as territorial governor with Alfred Cumming. The expedition was also known as the Utah War.
As fear of invasion grew, Mormon settlers had convinced some Paiute Indians to aid in a Mormon-led attack on 120 immigrants from Arkansas under the guise of Indian aggression. The murder of these settlers became known as the Mountain Meadows massacre. The Mormon leadership had adopted a defensive posture that led to a ban on the selling of grain to outsiders in preparation for an impending war. This chafed pioneers traveling through the region, who were unable to purchase badly needed supplies. A disagreement between some of the Arkansas pioneers and the Mormons in Cedar City led to the secret planning of the massacre by a few Mormon leaders in the area. Some scholars debate the involvement of Brigham Young. Only one man, John D. Lee, was ever convicted of the murders, and he was executed at the massacre site.
Express riders had brought the news 1,000 miles from the Missouri River settlements to Salt Lake City within about two weeks of the army's beginning to march west. Fearing the worst as 2,500 troops (roughly 1/3rd of the army then) led by General Albert Sidney Johnston started west, Brigham Young ordered all residents of Salt Lake City and neighboring communities to prepare their homes for burning and evacuate southward to Utah Valley and southern Utah. Young also sent out a few units of the Nauvoo Legion (numbering roughly 8,000–10,000), to delay the army's advance. The majority he sent into the mountains to prepare defenses or south to prepare for a scorched earth retreat. Although some army wagon supply trains were captured and burned and herds of army horses and cattle run off no serious fighting occurred. Starting late and short on supplies, the United States Army camped during the bitter winter of 1857–58 near a burned out Fort Bridger in Wyoming. Through the negotiations between emissary Thomas L. Kane, Young, Cumming and Johnston, control of Utah territory was peacefully transferred to Cumming, who entered an eerily vacant Salt Lake City in the spring of 1858. By agreement with Young, Johnston established the army at Fort Floyd 40 miles away from Salt Lake City, to the southwest.
Salt Lake City was the last link of the First Transcontinental Telegraph, between Carson City, Nevada and Omaha, Nebraska completed in October 1861. Brigham Young, who had helped expedite construction, was among the first to send a message, along with Abraham Lincoln and other officials. Soon after the telegraph line was completed, the Deseret Telegraph Company built the Deseret line connecting the settlements in the territory with Salt Lake City and, by extension, the rest of the United States.
Because of the American Civil War, federal troops were pulled out of Utah Territory (and their fort auctioned off), leaving the territorial government in federal hands without army backing until General Patrick E. Connor arrived with the 3rd Regiment of California Volunteers in 1862. While in Utah, Connor and his troops soon became discontent with this assignment wanting to head to Virginia where the "real" fighting and glory was occurring. Connor established Fort Douglas just three miles (5 km) east of Salt Lake City and encouraged his bored and often idle soldiers to go out and explore for mineral deposits to bring more non-Mormons into the state. Minerals were discovered in Tooele County, and some miners began to come to the territory. Conner also solved the Shoshone Indian problem in Cache Valley Utah by luring the Shoshone into a midwinter confrontation on January 29, 1863. The armed conflict quickly turned into a rout, discipline among the soldiers broke down, and the Battle of Bear River is today usually referred to by historians as the Bear River Massacre. Between 200 and 400 Shoshone men, women and children were killed, as were 27 soldiers, with over 50 more soldiers wounded or suffering from frostbite.
Beginning in 1865, Utah's Black Hawk War developed into the deadliest conflict in the territory's history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and Utah local militia.
On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the state, and several influential businessmen made fortunes in the territory.
Main article: Latter Day Saint polygamy in the late-19th century
During the 1870s and 1880s, federal laws were passed and federal marshals assigned to enforce the laws against polygamy. In the 1890 Manifesto, the LDS Church leadership dropped its approval of polygamy citing divine revelation. When Utah applied for statehood again in 1895, it was accepted. Statehood was officially granted on January 4, 1896.
The Mormon issue made the situation for women the topic of nationwide controversy. In 1870 the Utah Territory, controlled by Mormons, gave women the right to vote. However, in 1887, Congress disenfranchised Utah women with the Edmunds–Tucker Act. In 1867–96, eastern activists promoted women's suffrage in Utah as an experiment, and as a way to eliminate polygamy. They were Presbyterians and other Protestants convinced that Mormonism was a non-Christian cult that grossly mistreated women. The Mormons promoted woman suffrage to counter the negative image of downtrodden Mormon women. With the 1890 Manifesto clearing the way for statehood, in 1895 Utah adopted a constitution restoring the right of women's suffrage. Congress admitted Utah as a state with that constitution in 1896.
Though less numerous than other intermountain states at the time, several lynching murders for alleged misdeeds occurred in Utah territory at the hand of vigilantes. Those documented include the following, with their ethnicity or national origin noted in parentheses if it was provided in the source:
William Torrington in Carson City (then a part of Utah territory), 1859
Thomas Coleman (Black man) in Salt Lake City, 1866
3 unidentified men at Wahsatch, winter of 1868
A Black man in Uintah, 1869
Charles A. Benson in Logan, 1873
Ah Sing (Chinese man) in Corinne, 1874
Thomas Forrest in St. George, 1880
William Harvey (Black man) in Salt Lake City, 1883
John Murphy in Park City, 1883
George Segal (Japanese man) in Ogden, 1884
Joseph Fisher in Eureka, 1886
Robert Marshall (Black man) in Castle Gate, 1925
Other lynchings in Utah territory include multiple instances of mass murder of Native American children, women, and men by White settlers including the Battle Creek massacre (1849), Provo River Massacre (1850), Nephi massacre (1853), and Circleville Massacre (1866).
Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah began to become known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes, and such natural landmarks as Delicate Arch and "the Mittens" of Monument Valley are instantly recognizable to most national residents. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.
Beginning in 1939, with the establishment of Alta Ski Area, Utah has become world-renowned for its skiing. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world. Salt Lake City won the bid for the 2002 Winter Olympics in 1995, and this has served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues scattered across the Wasatch Front continue to be used for sporting events. This also spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the re-construction of the freeway system around the city.
During the late 20th century, the state grew quickly. In the 1970s, growth was phenomenal in the suburbs. Sandy was one of the fastest-growing cities in the country at that time, and West Valley City is the state's 2nd most populous city. Today, many areas of Utah are seeing phenomenal growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Transportation and urbanization are major issues in politics as development consumes agricultural land and wilderness areas.
In 2012, the State of Utah passed the Utah Transfer of Public Lands Act in an attempt to gain control over a substantial portion of federal land in the state from the federal government, based on language in the Utah Enabling Act of 1894. The State does not intend to use force or assert control by limiting access in an attempt to control the disputed lands, but does intend to use a multi-step process of education, negotiation, legislation, and if necessary, litigation as part of its multi-year effort to gain state or private control over the lands after 2014.
Utah families, like most Americans everywhere, did their utmost to assist in the war effort. Tires, meat, butter, sugar, fats, oils, coffee, shoes, boots, gasoline, canned fruits, vegetables, and soups were rationed on a national basis. The school day was shortened and bus routes were reduced to limit the number of resources used stateside and increase what could be sent to soldiers.
Geneva Steel was built to increase the steel production for America during World War II. President Franklin D. Roosevelt had proposed opening a steel mill in Utah in 1936, but the idea was shelved after a couple of months. After the attack on Pearl Harbor, the United States entered the war and the steel plant was put into progress. In April 1944, Geneva shipped its first order, which consisted of over 600 tons of steel plate. Geneva Steel also brought thousands of job opportunities to Utah. The positions were hard to fill as many of Utah's men were overseas fighting. Women began working, filling 25 percent of the jobs.
As a result of Utah's and Geneva Steels contribution during the war, several Liberty Ships were named in honor of Utah including the USS Joseph Smith, USS Brigham Young, USS Provo, and the USS Peter Skene Ogden.
One of the sectors of the beachhead of Normandy Landings was codenamed Utah Beach, and the amphibious landings at the beach were undertaken by United States Army troops.
It is estimated that 1,450 soldiers from Utah were killed in the war.
In the sixties, these towers were built in Antwerp as a new cityproject. They were ment to be state of the art modern architecture and should create a new kind of city. Unfortenately, the project didn't reached it's goals and instead of becomming the new and hip place to be, it became the opposite. How the mind of an architect can be to far ahead for society...
To get from Nice to London, I opted to fly on British Airways. A decade earlier, I was a BA Gold Card member. I booked this NCE-LHR without much enthusiasm, aware that the cheeseparing regime of former CEO Alex Cruz had imposed draconian cuts to the airline’s standards of comfort and service. The Economy Class seat-pitch had been tightened to an unacceptable 29 inches (Ryanair offers better) and food was strictly buy-on-board. So I forked out $672 for a 1-way Club Class ticket for a 31-inch seat pitch and free scoff. This was the food offering - OK, but nothing to excite the palate. The service was OK, but ditto: BA cabin staff can be friendly or totally aloof and even perfunctory. The flight was punctual and I had no issues with checked-in luggage. I give it a 7/10 rating, but I won’t rushing back to BA anytime soon.
YIPPPEE! the weekend's finally here, hope this starts it off on a bright note for you.
and a happy May two4 long weekend to all Canadian flickr'ites. it's the unofficial start of summer in the great white north, time to celebrate.
In the silence of the oncoming darkness on the shores of Yellowstone Lake, where coyotes cry out in the night, and solitary wolves howl to each other under the stars.
This photo was taken well after sunset on June 25, 2012 under a cloudless sky as the stars shone brightly.
Technical details: Canon EOS 5D Mark II, Sigma 20mm f/1.8 lens at ISO800, f/5.6, 30 sec.
In the middle of the flock of franklin's, one young gull was enjoying a refreshing bath.
1st Winter Franklin's gull (Leucophaeus pipixcan)
My photos can also be found at kapturedbykala.com
This is an entrance to an amazing building also located around Eureka Springs, AR. This is a very small portion to what enters into just a lovely building.
Everest Basecamp – mount everest, who does not know this mountain. The highest mountain in the world with a height of 8.848 meters (29,028 ft). who always wanted conguered mountain climbers climbers reliable. This mountain is deadly for novice climbers, so for those of you who are still a beginner, do not try to try to conguered this mountain. not necessarily because of his conguered climbers can reliably especially novice climbers.
The following is the Everest base camp
At Everest Base Camp, climbers will Often spend 4-8 weeks, acclimatizing to the altitude. During that time, the “Icefall Doctors” will set up ropes and ladders in the notoriously unstable Khumbu Icefall. Seracs, crevasses and shifting blocks of ice of make the icefall one of the most dangerous sections of the route. Many climbers and Sherpas have been killed in this section. To reduce the risk, climbers will usually begin Reviews their ascent well before sunrise when the freezing Temperatures glue ice blocks in place.Camp I
Above the icefall is Camp I at 6.065 m (19,900 ft) Camp 1 is mostly a temporary camp with most climbers just spending one night at this camp.Camp II
Base Camp II, Advanced Base Camp (ABC) is established at 6,400 m (21,300 ft). The Western Cwm is a are relatively flat, Gently rising glacial valley, marked by huge lateral crevasses in the center roomates Prevent direct access to the Upper Reaches of the Cwm. Climbers are forced to cross on the far right near the base of Nuptse to a small passageway known as the “Nuptse corner”. The Western Cwm as the topography of the area geneally cuts off wind from the climbing route. The high altitude and a clear, windless day can the make the Western Cwm unbearably hot for climbers.Camp III
From ABC, climbers ascend the Lhotse face on set of ropes up to Camp III, on small ledges situated at Approximately 7,200 m to 7,400 m. From there, it is another 500 meters to Camp IV on the South Col at 7.920 m (26,000 ft). From Camp III to Camp IV, mountaineers are faced with two additional obstacles: The “Geneva Spur” and the “Yellow Band”. The Geneva Spur is an anvil shaped rib of black rock named by a 1952 Swiss expedition. Fixed ropes help climbers in scrambling over this snow covered rock band. The Yellow Band is a section of sedimentary sandstone. The route from the base of the Lhotse face to the Summit is almost always completely fixed with static line.Camp IV
On the South Col, climbers are very close to 8,000 m and can only spend limited time at those altitudes even with supplemental oxygen. Climbers typically only have a maximum of two or three days they can tolerate at this altitude for making peak bids. Clear weather and low winds are important factors when Deciding on a summit attempt. If weather does not cooperate within Reviews These short few days, climbers are forced to move down, many all the way back down to Base Camp.
From Camp IV, mountaineers Reviews their summit push will start from 8 pm to 2 am with the hope of reaching the summit (still another 1,000 meters above) within 10 to 12 hours. Climbers will first reach “The Balcony” at 8,400 m (27,700 ft), a small platform where they can rest and gaze at peaks to the south and east in the early dawn light. Continuing up the ridge, climbers are then faced with a series of impressive rock steps the which usually forces them to the east into waist deep snow, a large amount of sudden grave hazard. At 8,750 m (28,700 ft), a small table-sized arena of ice and snow marks the South Summit.
From the South Peak, mountaineers go after the knife-edge along the Southeast Ridge the which is known as the “Cornice traverse” where snow griping to irregular rock. This is the most bare part of the climb as a misstep to the left would send one 2,400 m (8,000 ft) down the southwest face while to the immediate right is the 3,050 m (10,000 ft) Kangshung face. At the end of this traverse is an imposing 12 m (40 ft) rock wall called the “Hillary Step” at 8.760 m (28.750 ft).
Tenzing and Hillary were the first mountaineers to rise this step and they did it with prehistoric ice climbing equipment and without fixed ropes. Now, climbers will ascend this step using fixed ropes Previously set up by Sherpas. Once above the step, it is a comparatively easy climb to the top on fairly angled snow slopes – though the exposure on the ridge is extreme especially while traversing very large cornices of snow. After the Hillary Step, climbers must traverse Also a very loose and rocky section that has a very large entanglement of fixed ropes that can be troublesome in bad weather. Climbers will typically spend less than a half-hour on “top of the world” as they Realize the need to descend to Camp IV before darkness sets in, afternoon weather Becomes a serious problem, or supplemental oxygen tanks run out.
That Everest base camp you will visit when you are mountain climbing Everest. if you are big enough guts, you should climb this mountain. but if you are in doubt it is better not try to climb this mountain.
by New Hotel Travel in ift.tt/1q2Vh1i
in the spirit of collaboration.
Photography by marty.
Processing by me.
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Some days we do so much stuff, there's not enough space to post all the pictures I take.
Take Monday.
Monday was back at work day, a day of meetings and getting documents reviewed, but also I would go up to that London in the evening. For an event.
Sunday night we went to collect Jen's car so Jools had a car to drive to work, and I could go to the station after work.
That done, all was set.
Thing is, could I think of a good enough excuse not to go? Because as I get older, it seems easier to bail on things we have agreed to do, or even bought tickets for.
So, with banks of fog and mist sweeping over St Maggies through the day, I check train times to see if there were delays, or the weather to see if the weather would get worse after dark.
As it happens, despite fog and mist, trains kept running as normal. And there was no weather warnings for the evening either.
So, I worked through the day, looking out of the windows as the village faded from the view at times.
I would go I decided.
So, after the last meeting in the afternoon, I packed away the work computer and took the Audi to drive to Dover Priory, finding a place to park very near the station, much to my surprise.
A day return cost £37, so I bought that and went for a pasty and Coke in the buffet to wait.
A high speed train gets us to London in 63 minutes, and after that, a three stop ride on the Piccadilly Line to Leicester Square would take me to the centre of the west end where the action might possibly be.
The train wasn't full, only between Folkestone and Ashford when love-lorn school kids got on, gossiping about someone who might or might not fancy them.
Bless.
At Ashford the train even waited for a connection from the Marsh Line, something no longer thought happens.
But does.
And then on to London.
There really is no better station to arrive into London.
Not as busy as I have seen, but lots of people milling around with suitcases, ready to travel.
I was making my way to the Piccadilly Line for a short ride to Leicester Square and the bright lights of the west end.
Arriving at Leicester Square, I fine neon everywhere and a Christmas Market set up in the middle.
For the snapper, it was a target rich environment.
Across Leicester Square, and over Piccadilly Circus to look up the curving Regency masterpiece that is Regent Street, already decked out ready for Christmas.
Back and into Chinatown, where it was packed. I mean packed so there was people jams. Most were from the far east, it seemed, and always struck me as odd that they would come to England and eat on the same food as back home. But then little different to package holidaymakers from England going to Spain in the 1970, dining on fry up and egg and chips.
I walked to Trafalgar Square, bought a Cajun hot dog and a coke, and ate that sitting on a bench looking at the reflections in the fountain pools around Nelson's Column.
I saw St Martin in the Fields was open, so I went in. There were teccy looking people setting up mics for a concert, so I had little time, but rattled off a few shots before their icy glares drove me back outside.
Oddly, I wasn't that hungry, so snacked through the day.
I went to find the venue for the event, a pub on the backstreets behind theatreland, I had half an hour, so waited and watched people before going in for a beer.
The event was a "thank you" for patrons of the music podcast I support. Other patrons came from all over London and the country, a couple from Dublin came too.
A soundtrack of party tunes was playing in the upstairs bar, and my selection, What's my Scene by The Hoodoo Gurus was playing.
I meet some old familiar faces, we make small talk and jokes, most music based.
Sadly, I had to leave just before nine, as I had an audit first thing in the morning, and I really needed to catch the twenty to ten train back to Dover, even then it would be nearly ten to eleven before I got back to Dover, and then a ten minute drive home.
So, outside the pub I flag down a cab and he takes me up to St Pancras, so quickly I had twenty minutes to wait before departure, indeed the train wasn't even waiting when I went up from street level.
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St Martin-in-the-Fields is a Church of England parish church at the north-east corner of Trafalgar Square in the City of Westminster, London. It is dedicated to Saint Martin of Tours. There has been a church on the site since at least the medieval period. It was at that time located in the farmlands and fields beyond the London wall, when it was awarded to Westminster Abbey for oversight.
It became a principal parish church west of the old City in the early modern period as Westminster's population grew. When its medieval and Jacobean structure was found to be near failure, the present building was constructed in an influential neoclassical design by James Gibbs in 1722–1726. The church is one of the visual anchors adding to the open-urban space around Trafalgar Square.
Excavations at the site in 2006 uncovered a grave from about A.D. 410.[3] The site is outside the city limits of Roman London (as was the usual Roman practice for burials) but is particularly interesting for being so far outside (1.6 km or 1 statute mile west-south-west of Ludgate), and this is leading to a reappraisal of Westminster's importance at that time. The burial is thought by some to mark a Christian centre of that time (possibly reusing the site or building of a pagan temple
The earliest extant reference to the church is from 1222, when there was a dispute between the Abbot of Westminster and the Bishop of London as to who had control over it. The Archbishop of Canterbury decided in favour of Westminster, and the monks of Westminster Abbey began to use it.[4]
Henry VIII rebuilt the church in 1542 to keep plague victims in the area from having to pass through his Palace of Whitehall. At this time it was literally "in the fields", occupying an isolated position between the cities of Westminster and London.
By the beginning of the reign of James I, the local population had increased greatly and the congregation had outgrown the building. In 1606 the king granted an acre (405 m²) of ground to the west of St Martin's Lane for a new churchyard,[5] and the building was enlarged eastwards over the old burial ground, increasing the length of the church by about half.[6] At the same time, the church was, in the phrase of the time, thoroughly "repaired and beautified".[6] Later in the 17th century, capacity was increased by the addition of galleries. The creation of the new parishes of St Anne, Soho, and St James, Piccadilly, and the opening of a chapel in Oxenden Street also relieved some of the pressure on space.[5]
As it stood at the beginning of the 18th century, the church was built of brick, rendered over, with stone facings. The roof was tiled, and there was a stone tower, with buttresses. The ceiling was slightly arched,[6] supported with what Edward Hatton described as "Pillars of the Tuscan and Modern Gothick orders".[6] The interior was wainscotted in oak to a height of 6 ft (1.8 m), while the galleries, on the north, south and west sides, were of painted deal.[6] The church was about 84 ft (26 m) long and 62 ft (19 m) wide. The tower was about 90 ft (27 m) high.[6]
A number of notables were buried in this phase of the church, including Robert Boyle, Nell Gwyn, John Parkinson and Sir John Birkenhead.
A survey of 1710 found that the walls and roof were in a state of decay. In 1720, Parliament passed an act for the rebuilding of the church allowing for a sum of up to £22,000, to be raised by a rate on the parishioners. A temporary church was erected partly on the churchyard and partly on ground in Lancaster Court. Advertisements were placed in the newspapers that bodies and monuments of those buried in the church or churchyard could be taken away for reinterment by relatives.
The rebuilding commissioners selected James Gibbs to design the new church. His first suggestion was for a church with a circular nave and domed ceiling,[7] but the commissioners considered this scheme too expensive. Gibbs then produced a simpler, rectilinear plan, which they accepted. The foundation stone was laid on 19 March 1722, and the last stone of the spire was placed into position in December 1724. The total cost was £33,661 including the architect's fees.[5]
The west front of St Martin's has a portico with a pediment supported by a giant order of Corinthian columns, six wide. The order is continued around the church by pilasters. In designing the church, Gibbs drew upon the works of Christopher Wren, but departed from Wren's practice in his integration of the tower into the church. Rather than considering it as an adjunct to the main body of the building, he constructed it within the west wall, so that it rises above the roof, immediately behind the portico,[7] an arrangement also used at around the same time by John James at St George, Hanover Square (completed in 1724), although James' steeple is much less ambitious.[7] The spire of St Martin's rises 192 ft (59 m) above the level of the church floor.[5]
The church is rectangular in plan, with the five-bay nave divided from the aisles by arcades of Corinthian columns. There are galleries over both aisles and at the west end. The nave ceiling is a flattened barrel vault, divided into panels by ribs. The panels are decorated in stucco with cherubs, clouds, shells and scroll work, executed by Giuseppe Artari and Giovanni Bagutti.[5]
Until the creation of Trafalgar Square in the 1820s, Gibbs's church was crowded by other buildings. J. P. Malcolm, writing in 1807, said that its west front "would have a grand effect if the execrable watch-house and sheds before it were removed" and described the sides of the church as "lost in courts, where houses approach them almost to contact".[8]
The design was criticised widely at the time, but subsequently became extremely famous, being copied particularly widely in the United States.[9] Although Gibbs was discreetly Catholic, his four-wall, long rectangular floor plan, with a triangular gable roof and a tall prominent centre-front steeple (and often, columned front-portico), became closely associated with Protestant church architecture world-wide.[10] In Britain, the design of the 1730s St Andrew's in the Square church in Glasgow was inspired by it. In India, St Andrew's Church, Egmore, Madras (now Chennai), is modelled on St Martin-in-the-Fields. In South Africa, the Dutch Reformed Church in Cradock is modelled on St Martin-in-the-Fields.
Various notables were soon buried in the new church, including the émigré sculptor Louis-François Roubiliac (who had settled in this area of London) and the furniture-maker Thomas Chippendale (whose workshop was in the same street as the church, St Martin's Lane[11]), along with Jack Sheppard in the adjoining churchyard. This churchyard, which lay to the south of the church, was removed to make way for Duncannon Street, constructed in the 19th century to provide access to the newly created Trafalgar Square.[12] Two small parcels of the churchyard survived, to the north and east of the church. The Metropolitan Public Gardens Association laid them out for public use in 1887; unusually for the MPGA, it paved them with flagstones as well as planted them with trees. For many years covered in market stalls, the churchyard has been restored including with the provision of seating.[13]
Before embarking for the Middle East Campaign, Edmund Allenby was met by General Beauvoir De Lisle at the Grosvenor Hotel and convinced General Allenby with Bible prophecies of the deliverance of Jerusalem. He told General Allenby that the Bible said that Jerusalem would be delivered in that very year, 1917, and by Great Britain. General Beauvoir de Lisle had studied the prophecies, as he was about to preach at St Martin-in-the-Fields.
Marsala (Maissala in sicilian; Lilybaeum in Latin) is an Italian town located in the Province of Trapani in the westernmost part of Sicily. Marsala is the most populous town in Trapani, and the fifth-highest in Sicily.
The town is famous for the landing of Garibaldi on 11 May 1860 (the Expedition of the Thousand) and for its Marsala wine. A feature of the area is the natural reserve of Stagnone Lagoon—a marine area with salt ponds.
Marsala is built on the ruins of the ancient Carthaginian city Lilybaion, and includes the archaeological site of Motya island, an ancient Phoenician town.
(Wikipedia)
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Salt evaporation ponds area north of Marsala is a must see for those seeking for beautiful and tranquil places - have been there twice, in the morning and in the evening, and both the visits of this charming place were really worth of.
Probably my favourite pic of the bunch. It shows the squad in action, except for the driver who I couldn't fit in the cab ;). The sniper is at the hatch on top.
Another natures's beauty in God's own country, Kerala. Water from Vazhachal (another beautiful waterfalls) flows as a small river for 3km before culminating in this amazing fall. As it is summer the water quantity was less. I took this photo from a distance of using a telephoto lens.
Kaohsiung
Ferry
Taiwan
2013
Life in and around public transport
Nikon D7100 + 35mm 1.8
Latest blogpost: thecovertphotographer.wordpress.com
©All photographs on this site are copyright: ©DESPITE STRAIGHT LINES (Paul Williams) 2011 – 2021 & GETTY IMAGES ®
No license is given nor granted in respect of the use of any copyrighted material on this site other than with the express written agreement of ©DESPITE STRAIGHT LINES (Paul Williams). No image may be used as source material for paintings, drawings, sculptures, or any other art form without permission and/or compensation to ©DESPITE STRAIGHT LINES (Paul Williams)
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Photograph taken at an altitude of Forty nine metres at 09:45am on Saturday 20th February 2021 off Blackheath Avenue and Charlton Way in the grounds of Greenwich Park, one of the Royal Parks of London situated in Greenwich, South East London.
The carrion crow (Corvus corone) is a passerine bird of the family Corvidae and the genus Corvus which is native to western Europe and eastern Asia. It can grow to twenty inches in length with a wingspan of up to thirty nine inches. Highly intelligent, utterly beautiful with an amazingly detailed and rich plumage, these stunning birds are much maligned and tainted with unfair tags attributed through folklore and ignorance. I love 'em!
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Nikon D850 Hand held with Sigma OS Optical Stabilization enabled on normal setting. Focal length 420mm Shutter speed: 1/250s Aperture f/6.0 ISO640 Image area FX (36 x 24) NEF RAW L (8256 x 5504). NEF RAW L (14 bit uncompressed) Focus mode AF-C focus. AF-C Priority Selection: Release. Nikon Back button focusing enabled. Auto ISO 3D Tracking watch area: Normal 55 Tracking points.AF-Area mode single point & 73 point switchable. Exposure mode: Shutter priority mode. Matrix metering. White balance on: Auto1 (4370K). Colour space: RGB. Vignette control: Normal. Picture control: Auto (Sharpening A +1/Clarity A+1)
Sigma 60-600mm f/4.5-6.3DG OS HSM SPORTS. Lee SW150 MKI filter holder with MK2 light shield and custom made velcro fitting for the Sigma lens. Lee SW150 circular polariser glass filter.Lee SW150 Filters field pouch.Nikon GP-1 GPS module. Hoodman HEYENRG round eyepiece oversized eyecup.Mcoplus professional MB-D850 multi function battery grip 6960.Two Nikon EN-EL15a batteries (Priority to battery in Battery grip). Black Rapid Curve Breathe strap. My Memory 128GB Class 10 SDXC 80MB/s card. Lowepro Flipside 400 AW camera bag.
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LATITUDE: N 51d 28m 29.18s
LONGITUDE: E 0d 0m 17.70s
ALTITUDE: 49.0m
RAW (TIFF) FILE: 130.00MB NEF: 94.4MB
PROCESSED (JPeg) FILE: 48.50MB
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PROCESSING POWER:
Nikon D850 Firmware versions C 1.20 (14/01/2021) LD Distortion Data 2.018 (18/02/20) LF 1.00
HP 110-352na Desktop PC with AMD Quad-Core A6-5200 APU 64Bit processor. Radeon HD8400 graphics. 8 GB DDR3 Memory with 1TB Data storage. 64-bit Windows 10. Verbatim USB 2.0 1TB desktop hard drive. WD My Passport Ultra 1tb USB3 Portable hard drive. Nikon ViewNX-1 64bit Version 1.4.1 (18/02/2020). Nikon Capture NX-D 64bit Version 1.6.2 (18/02/2020). Nikon Picture Control Utility 2 (Version 2.4.5 (18/02/2020). Nikon Transfer 2 Version 2.13.5. Adobe photoshop Elements 8 Version 8.0 64bit.
In Ballarat a ghost Town in Death Valley, A very old man have a shop. He have many life and story to tell...
Dans Ballarat, une ville fantôme dans la Vallée de la Mort, un vieil homme tient une boutique. Il est plein de vie et d'histoires du passé. Son accent est par contre difficile a comprendre, il doit penser la même chose de moi :-)
Ballarat at Death Valley, California, USA