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Topic: Geology of the Bryce Canyon area

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Bryce Canyon National Park

Geology of the Grand Canyon area

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Bryce Canyon

	Bryce Canyon National Park - Wikipedia, the free encyclopedia
		The canyon area was settled by Mormon pioneers in the 1850s and was named after Ebenezer Bryce, who homesteaded in the area in 1875.
		Bryce Canyon was not formed from erosion initiated from a central stream, meaning it technically is not a canyon.
		Bryce grazed his cattle inside what are now park borders and reputedly thought that the amphitheaters were a "helluva place to lose a cow." He also built a road to the plateau to retrieve firewood and timber and a canal to irrigate his crops and water his animals.
	www.wikipedia.org /wiki/Bryce_Canyon (2973 words)

	Geology of the Zion and Kolob canyons area - Wikipedia, the free encyclopedia
		The geology of the Zion and Kolob canyons area includes nine known exposed formations, all visible in Zion National Park in the state of Utah in the United States, and representing about 150 million years of mostly Mesozoic-aged sedimentation.
		This means that the oldest strata are exposed along the Virgin River in the Zion Canyon part of the park, and the youngest are exposed in the Kolob Canyons section.
		Bryce Canyon National Park to the northeast continues where the Zion and Kolob area end by presenting Cenozoic-aged rocks (see geology of the Bryce Canyon area).
	en.wikipedia.org /wiki/Geology_of_the_Zion_and_Kolob_canyons_area (2533 words)

	Geology of the Bryce Canyon area - Wikipedia, the free encyclopedia
		The exposed geology of the Bryce Canyon area shows a record of deposition that covers the last part of the Cretaceous period and the first half of the Cenozoic era in that part of North America.
		The ancient depositional environment of the region around what is now Bryce Canyon National Park varied from the warm shallow sea in which the Dakota Sandstone and the Tropic Shale were deposited to the cool streams and lakes that contributed to the colorful Claron Formation that dominates the park's amphitheaters.
		In the Bryce Canyon area this formation can be seen in the Paria Valley where it is found as a lithified blanket sand that probably accumulated on beaches, in lagoons, and in coal swamps as the Cretaceous Seaway transgressed (advanced inland) over the region.
	en.wikipedia.org /wiki/Geology_of_the_Bryce_Canyon_area (1015 words)

	Bryce Canyon National Park - Wikipedia, the free encyclopedia
		Bryce is distinctive due to its unique geological structures, called hoodoos, formed from wind, water, and ice erosion of the river and lakebed sedimentary rocks.
		The Bryce Canyon area shows a record of deposition that spans from the last part of the Cretaceous period and the first half of the Cenozoic era.
		The lowest areas of the park are dominated by dwarf forests of pinyon pine and juniper with manzanita, serviceberry, and antelope bitterbrush in between.
	en.wikipedia.org /wiki/Bryce_Canyon_National_Park (2973 words)

	Bryce Canyon National Park
		Due to geology in the area, uplift and erosion has occurred, leaving behind Hoodoos and many other beautiful formations with oranges and red colors.
		Bryce National Park, Zion National Park, and Cedar Breaks all have undergone the similar geology.
		Bryce Canyon was set aside in 1923 by President Warren G. Harding a national monument.
	geology.csusb.edu /vtrips/ynp/bryce.htm (501 words)

	Bryce Canyon (Site not responding. Last check: 2007-09-06)
		As the Paleocene progressed, the interior seaway began to drain, and the marine waters receded from the foot of the Sevier orogenic belt to the east permanently.
		The region that is Bryce Canyon, however, was not uplifted until after the Oligocene (~35 mya), when there was extensive volcanic activity throughout southwestern Utah.
		Bryce Canyon is located on one of these plateaus, called the Paunsaugunt Plateau.
	www.oberlin.edu /Geopage/projects/204projects/mausner/Bryce_Canyon.html (705 words)

	Bryce Canyon National Park : A Nature Guide : Landscape & Geology \| Frommers.com
		Named for the Colorado River, which is responsible for carving many of the area's scenic canyons, the Colorado Plateau began as the result of uplifting 10 to 15 million years ago.
		Much of Bryce Canyon's rock is limestone, relatively soft and crumbly, which was easily eroded into the park's numerous intricate hoodoos.
		Most of the rocks at Zion and Bryce Canyon are colored by iron, or hematite (iron oxide), either contained in the original stone or carried into the rocks by groundwater.
	www.frommers.com /destinations/brycecanyonnationalpark/1561026075.html (938 words)

	The Geology of the Grand Canyon
		Other forces that contributed to the Canyon's formation are the course of the Colorado River itself, vulcanism, continental drift and slight variations in the earths orbit which in turn causes variations in seasons and climate.
		The area from Bryce Canyon down to Grand Canyon is typically referred to as the Grand Staircase.
		Side canyons had formed along fault lines in the rock and these were eroded away and the rock within them carried down to the Colorado.
	www.kaibab.org /geology/gc_geol.htm (3443 words)

	bryce canyon np (Site not responding. Last check: 2007-09-06)
		Bryce Canyon National Park, located in southcentral Utah, was first explored by Capt. Clarence E. Dutton and John Wesley Powell in the 1870s.
		Many of the names in the area are derived from the Paiute language, of the Paiute Native Americans that lived in the area.
		The Paiutes were later moved by the Mormons that came in the Paria Valley (where Bryce Canyon is located), and in 1875 Ebenezer Bryce started developing communities in southcentral Utah and nothern Arizona.
	www.ux1.eiu.edu /~cfrbj/parks/brca/brcanp.htm (299 words)

	Bryce Canyon National Park
		You then will be able to view activities in Bryce Canyon National Park, Utah by category which include horseback riding, ATV tours, air tours, biking, entertainment, fishing, golf, guided tours, hunting, museums, paintball, ranch activities, rappelling, river running, shopping, snowmobiling and skiing.
		Bryce Canyon National Park, Utah is named for just one of many canyons which form a series of horseshoe-shaped amphitheaters on the edge of the Paunsaugunt Plateau in southern Utah.
		Bryce Canyonn Inn is your best choice for visiting the parks and monuments of Southern Utah and Northern Arizona.
	www.travelwest.net /parks/brycecanyon (555 words)

	Bryce Canyon - Location / Itineraries
		Bryce Canyon - At the gate you will be given a map of the park.
		The main road in Bryce Canyon goes from the Gate on the North for 18 miles to the South end of the park.
		Anciently there were many geysers in this area that, over time ceased to spew water from their natural rock pipes within the ground.
	www.brycecanyonresort.com /bryce-canyon-location.html (1906 words)

	Bryce Canyon National Park: Description - DesertUSA
		Bryce Canyon National Park is a series of huge natural amphitheaters carved into sedimentary rocks by the Paria River and its tributaries, along the edge of the Paunsagunt Plateau.
		The canyon behind his home came to be known as Bryce's Canyon; today it remains the name of both a specific canyon and the national park.
		Bryce Canyon's forests and meadows support diverse animal life from small mammals and birds to foxes, mountain lions and fl bears.
	www.desertusa.com /bryce/du_bry_desc.html (768 words)

	Bryce Canyon National Park: Climate, Geography, Map (DesertUSA)
		Bryce Canyon National Park is about 80 miles northeast of Zion National Park but is starkly different in climate, topography, geology and scenery.
		Bryce sits atop the Paunsagunt Plateau of southwestern Utah between the Markagunt Plateau to the west and Aquarius Plateau to the east.
		Bryce Canyon National Park is 24 miles southeast of Panguitch, Utah.
	www.desertusa.com /bryce/du_bry_map.html (418 words)

	Bryce Canyon National Park - Biocrawler definition:Bryce Canyon National Park - Biocrawler (Site not responding. Last check: 2007-09-06)
		The largest is 12 mile (19 km) long, 3 mile (4.8 km) wide and 800 foot (240 m) deep Bryce Amphitheater.
		Bryce grazed his cattle inside what are now park borders and reputedly thought that the amphitheaters were a "helluva place to lose a cow.".
		He also built a road to the plateau to retrieve firewood and timber and a canal to irrigate his crops and water his animals.
	www.biocrawler.com /biowiki/Bryce_Canyon_National_Park (2974 words)

	Bryce Canyon Scenic ATV and Guided Tours
		Bryce Canyon Tours and ATV Adventures is very proud to offer three very distinct ways for you to enjoy Bryce Canyon Country and Southern Utah.
		Whatever your preference, Bryce Canyon Tours and ATV Adventures can and will give you the experience you are looking for.
		The information pertaining to the geology, flora, fauna, and history was shared in such a way that all understood and came to appreciate the beauty and wonder of the area.
	www.brycetours.com (220 words)

	Bryce Canyon National Park Information Guide
		Bryce Canyon National Park consists of 37,277 acres of scenic colorful rock formations and desert wonderland.
		Bryce Canyon National Park is named for one of a series of horseshoe-shaped amphitheaters carved from the eastern edge of the Paunsaugunt Plateau in southern Utah.
		Bryce Canyon's forest and meadows support diverse animal life, from small mammals and birds, to foxes and occasional mountain lion and fl bears.
	www.bryce.canyon.national-park.com /info.htm (1683 words)

	Bryce Canyon geology - geology bryce - geology bryce canyon national park
		Long ago and changing over the great spans of time the rocky area of of Bryce Canyon was once covered by sea, mountains, desert and costal plain.
		The hoodoos of Bryce Canyon are 60 million year old sculpted claron rock formations which consist of limestone, dolomite and siltstone layers.
		In Bryce Canyon it freezes at night approximately 360 days of the year, so this is occurring continuously.
	zionnational-park.com /bgeology.htm (995 words)

	Bryce Canyon National Park. Bryce Canyon national park, Bryce Canyon,national parks, Bryce, utah parks, utah, southern ...
		Bryce Canyon National Park is named for just one of many canyons which form a series of horseshoe-shaped amphitheaters on the edge of the Paunsaugunt Plateau in southern Utah.
		You'll want to make sure you visit when the weather is good, so visit Utah Weather.net for both Bryce Canyon weather information and other city and park weather in Utah.
		Open all year and located in the valley of Bryce Canyon on scenic Highway 12, Bryce Canyonn Inn is your best choice for visiting the parks and monuments of Southern Utah and Northern Arizona.
	www.brycecanyon.com (266 words)

	GORP - Bryce Canyon National Park, Utah - Environment
		Bryce Canyon is not a canyon at all, but a spectacular amphitheater carved by erosion in the 50 to 60 million year old rocks of the Pink cliffs.
		Zion Canyon is incised into the rock of the White Cliffs.
		The southern edge of the Kaibab Plateau is the north rim of the Grand Canyon, and this top edge of the Grand Canyon is the bottom of the Grand Staircase.
	gorp.away.com /gorp/resource/us_national_park/ut/env_bc.htm (1096 words)

	Zion National Park
		Zion is also known for its incredible slot canyons, including "The Narrows," which attract hikers from around the world.
		As a natural drainage for the area, the Virgin River carries flash floods during summer thunderstorms.
		Never enter narrow canyons if there is a chance of rain anywhere in the drainage.
	www.utah.com /nationalparks/zion.htm (845 words)

	Bryce Canyon National Park : Exploring the Area : Organized Tours \| Frommers.com
		Topics vary, but could include such subjects as the animals and plants of the park, geology, and the role of humans in the park's early days.
		Several times a week, spring through fall, usually in the evening, a talk is given on the patio or in the auditorium at Bryce Canyon Lodge.
		The free talks often include some lodge history, geology of the area, and discussion of some of the park's trails.
	www.frommers.com /destinations/brycecanyonnationalpark/1561023943.html (413 words)

	Bryce Canyon National Park
		Although it is the smallest of Utah's national parks at 35,835 acres, Bryce Canyon contains an outsized number of some of the most beautiful, unlikely rock formations on earth.
		Ponderosa pines, high-elevation meadows, and fir-spruce forests border the rim of this canyon on the Paunsaugunt Plateau.
		Canyon Trail Rides leads two-hour and half-day horse and mule rides in the spring, summer and fall.
	gorp.away.com /gorp/resource/us_national_park/ut_bryce.htm (967 words)

	About Bryce Canyon National Park
		Bryce Canyon is a wonderful and unique place that can take years to explore, yet you can gain a glimpse of the park's special wonders in a short time.
		Moonlight, sunrise, sunset and even rain and snow storms each create different moods over the amphitheaters at Bryce Canyon, whose hoodoos are the result of millions of years of erosion.
		Local people called the canyon with strange rock formations near Ebenezer's home "Bryce's Canyon." The Bryces moved to Arizona in 1880; to this day people continue to call this area Bryce Canyon.
	www.utahparks.com /national/bryce/about.html (388 words)

	Geology of Bryce and Public Attraction Info.
		The geology of Bryce Canyon is a study rich with change and the exciting interaction between nature's forces.
		As the area began to rise, the Paria and its tributaries underwent a dramatic change in steepness, becoming fast-moving, and therefore, became a powerful erosive force.
		While the water's role shapes the spires and pinnacles of Bryce Canyon with an average annual rainfall of only 16 inches, the cold nighttime temperatures on the plateau further chisels the landscape with over 200 freeze-thaw cycles annually on south-facing slopes.
	www1.infowest.com /lis/Bryce-Canyon/geology.html (731 words)

	Western Interior Seaway (Site not responding. Last check: 2007-09-06)
		The clam had a thick shell paved with "prisms" of calcite deposited perpendicular to the surface, which gave it a pearly luster in life.
		Paleontologists suggest that the giant size was an adaptation for life in the murky bottom waters, where a correspondingly large gill area would have allowed the animal to cope with oxygen-depleted waters.
		At the end of the Cretaceous continuing uplift in a mountain-building episode called the Laramide orogeny hoisted the sandbanks (sandstone) and muddy brackish lagoons (shale), the thick sequences of silt and sandstone still seen today as the Laramie Formation, while low-lying basins between them gradually subsided.
	www.infothis.com /find/Western_Interior_Seaway (474 words)

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