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178:. An even greater number of tributaries flow in from the north and east, including Death Hollow and Calf Creeks, the combined Boulder and Deer Creeks, The Gulch, Wolverine and Silver Falls Creeks, and Choprock, Moody, Stevens, and Cow Canyons. Streams from the north flow from
143:. The Escalante River begins at the confluence of Birch Creek and North Creek, with the flow of Pine Creek added just below the town. The river runs a total distance of 80 mi (130 km) from the Birch/North Creek confluence before emptying into the
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103:. This area—extending over 1,500 square miles (3,885 km) and rising in elevation from 3,600 ft (1,097 m) to over 11,000 ft (3,353 m)—is one of the three main sections of the
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layer. Due to the tilting of layers throughout the area, sandstone exposed at higher elevations near the town of
Escalante (e.g. Deer Creek) may be from a lower layer,
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170:, and Fiftymile Creek, along with the smaller Phipps, Fence, and Scorpion, Davis, Clear, and Indian Creeks. Most of these larger creeks flow from the top of the
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period, about 80 million years ago, the entire western section of North
America entered an era of uplift and mountain-building, an event known as the
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Numerous side canyons also feed the main river, accounting for the large size of the basin. From the west, the major tributaries are
411:. Millennium Science & Engineering, Inc. and Pocket Water Inc. August 26, 2005. p. 8 (of PDF; page 4 of original document).
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to the extent that erosional solid forces were acting on the
Escalante River Basin. Wetter climates during the recent
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era, 180 to 225 million years ago, when this area was part of a large area of dunes. Near the end of the
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237:. The lighter sandstone domes of Dance Hall Rock and Sooner Rocks are formed from the higher
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The sandstone layers now exposed in the
Canyons of the Escalante were deposited during the
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Sandstone exposed in canyons nearer to the
Colorado River is typically from the
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447:"Groundwater Discharge from the Navajo Sandstone in the Escalante Basin"
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The headwaters of the
Escalante River are located on the slopes of the
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233:. The dark red cliffs of Coyote Gulch, for example, are composed of
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and its tributaries—the
Escalante River Basin. Located in southern
487:
Geologic Map of
Capitol Reef National Park and vicinity (large PDF)
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402:"Escalante River Watershed Water Quality Management Plan (PDF)"
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period contributed to the deep cutting of the canyon walls.
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Location of the
Canyons of the Escalante within Utah
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214:province. These episodes of uplift raised the
210:. More recently, additional uplift formed the
151:. The lower section of the river, southeast of
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8:
760:Canyons and gorges of Garfield County, Utah
755:Grand Staircase–Escalante National Monument
598:Grand Staircase–Escalante National Monument
515:Canyon Hiking Guide to the Colorado Plateau
289:Canyon walls and stream-bed in Coyote Gulch
105:Grand Staircase–Escalante National Monument
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174:or from the base of its eastern edge, the
91:containing temporary rainwater deposits),
16:Erosional landforms in Utah, United States
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166:, Twentyfive Mile Creek, Coyote Gulch,
418:from the original on November 10, 2016
383:- only paved highway through the basin
7:
377:- unpaved access road to the canyons
109:Glen Canyon National Recreation Area
75:in the western United States, these
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530:, Trails Illustrated Map (1994),
369:Geology of the Capitol Reef area
363:Geology of the Bryce Canyon area
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274:Stevens Arch, near the mouth of
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155:, is now beneath the surface of
517:, by Michael R. Kelsey (1995),
79:features include high vertical
765:Landforms of Kane County, Utah
714:DomĂnguez–Escalante expedition
504:, by Rudi Lambrechtse (1985),
1:
562:History of the Escalante area
63:is a collective name for the
476:Escalante Canyon at utah.com
115:being adjacent to the east.
139:, just west of the town of
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750:Canyons and gorges of Utah
453:. BLM. n.d. Archived from
371:- to the east of the basin
365:- to the west of the basin
188:Capitol Reef National Park
113:Capitol Reef National Park
101:natural arches and bridges
87:, waterpockets (sandstone
693:Straight Cliffs Formation
176:Straight Cliffs Formation
107:, and also a part of the
67:landforms created by the
653:Canyons of the Escalante
528:Canyons of the Escalante
61:Canyons of the Escalante
719:Hole in the Rock Trail
375:Hole in the Rock Trail
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726:Xylorhiza cronquistii
683:Kaiparowits Formation
342:Video of Spooky Gulch
341:
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54:
502:Hiking the Escalante
457:on February 15, 2008
688:Kaiparowits Plateau
381:Utah State Route 12
172:Kaiparowits Plateau
33: /
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37:37.428°N 110.981°W
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698:Wahweap Formation
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243:Wingate Sandstone
239:Entrada sandstone
231:Glen Canyon Group
55:Calf Creek Canyon
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648:Aquarius Plateau
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235:Navajo Sandstone
216:Aquarius Plateau
212:Colorado Plateau
208:Laramide orogeny
184:Waterpocket Fold
180:Boulder Mountain
133:Aquarius Plateau
83:walls, numerous
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42:37.428; -110.981
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69:Escalante River
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145:Colorado River
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663:Devils Garden
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678:Horse Canyon
658:Death Hollow
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632:Willis Creek
612:Coyote Gulch
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496:Bibliography
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461:November 10,
459:. Retrieved
455:the original
450:
441:
432:
422:November 10,
420:. Retrieved
409:deq.utah.gov
408:
396:
313:Spooky Gulch
276:Coyote Gulch
262:Zebra Canyon
228:
197:
161:
153:Coyote Gulch
135:, in Utah's
130:
85:slot canyons
60:
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18:
627:Paria River
622:Harris Wash
301:Neon Canyon
224:Pleistocene
164:Harris Wash
157:Lake Powell
149:Kane County
89:depressions
40: /
28:110°58′52″W
744:Categories
451:ut.blm.gov
388:References
204:Cretaceous
25:37°25′41″N
141:Escalante
119:Geography
77:sandstone
65:erosional
552:Utah.com
413:Archived
347:See also
220:ice ages
200:Mesozoic
641:Geology
556:archive
249:Gallery
222:of the
194:Geology
111:, with
97:hoodoos
534:
521:
508:
81:canyon
707:Other
416:(PDF)
405:(PDF)
93:domes
532:ISBN
519:ISBN
506:ISBN
463:2016
424:2016
73:Utah
59:The
550:at
186:in
147:in
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449:.
407:.
245:.
190:.
159:.
99:,
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590:e
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554:(
465:.
426:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
