31:
469:
Nilsen, T. H.; Moore, T. E.; Dutro, J. T., Jr.; Brosgé, W. P. and
Orchard, D. M. (1980) "Sedimentology and Stratigraphy of the Kanayuk Conglomerate and Associated Units, Central and Eastern Brooks Range, Alaska: Report of the 1978 Field Season" United States Geological Survey Open file Report OF
244:
From south to north the
Endicott Mountains present long, broad glaciated valleys with rounded hills between rising in the center of the range to steep tors and aretes. The northern slopes of the Endicotts are steeper and more heavily incised, before they give way to the Arctic Coastal Plain.
209:. They are located in the middle of the Brooks range and run some 151 miles (243 km) east–west. To the east are the Philip Smith Mountains and to the west are the Schwatka Mountains. The Endicott Mountains are separated from the Philip Smith Mountains by the Middle Fork of the
385:. Above these are middle Cambrian sediments and the well documented Kanayuk Conglomerate. The Kanayuk Conglomerate is a fluvial deposit, made by a river in its flood plain, and can be up to 8,000 feet (2,400 m) thick. The Kanayuk Conglomerate began to be deposited in the
459:
Nilsen, T. H.; Moore, T. E.; Brosgé, W. P. and Dutro, J. T., Jr. (1981) "Sedimentology and
Stratigraphy of the Kanayut Conglomerate and Associated Units, Brooks Range, Alaska: Report of the 1981 Field Season" United States Geological Survey Open file Report OF
449:
Nilsen, T. H.; Moore, T. E.; Balin, D. F. and
Johnson, S. Y. (1982) "Sedimentology and Stratigraphy of the Kanayut Conglomerate, Central Brooks Range, Alaska—Report of 1980 Field Season" United States Geological Survey Open file Report OF
426:
Nilsen, T. H. and Moore, T. E. (1982) "Sedimentology and
Stratigraphy of the Kanayuk Conglomerate, Central and Western Brooks Range, Alaska—Report of the 1981 Field Season" United States Geological Survey Open file Report OF
563:
558:
436:
Nilsen, T. H. and Moore, T. E. (1984) "Stratigraphic
Nomenclature for the Upper Devonian and Lower Mississippian(?) Kanayuk Conglomerate, Brooks Range, Alaska"
568:
573:
160:
233:. The Endicott Mountains are separated from the mountains north of the Schwatka by Lucky Six Creek, Gull Pass, Gull Creek, a portion of the
71:
222:
503:
414:
393:. It is believed to have formed a huge delta almost 500 miles (800 km) long and 30 miles (48 km) wide.
495:
153:
64:
521:
Sedimentology and structural geology of the
Endicott Mountains allochthon, central Brooks Range, Alaska
519:
413:
as well as on the
Chandler Lake, Killik River, Survey Pass and Wiseman topographic maps of the
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8:
371:
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30:
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374:
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218:
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221:. The Endicott Mountains are separated from the Schwatka Mountains by
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386:
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54:
494:(6th edition) Kendall/Hunt Publishing Company, Dubuque, Iowa,
359:
as well as a number of unnamed peaks over 7000 ft.
333:Sillyasheen Mountain at 6,188 feet (1,886 m)
545:
314:Mount Arthur Emmons at 6,556 feet (1,998 m)
336:Bluecloud Mountain at 5,903 feet (1,799 m)
283:Cockedhat Mountain at 7,410 feet (2,259 m)
564:Landforms of Yukon–Koyukuk Census Area, Alaska
559:Gates of the Arctic National Park and Preserve
330:Mayukuit Mountain at 6,240 feet (1,902 m)
317:Rumbling Mountain at 6,510 feet (1,984 m)
569:Mountains of Northwest Arctic Borough, Alaska
348:Plateau Mountain at 5,322 feet (1,622 m)
311:Boreal Mountain at 6,654 feet (2,028 m)
253:Peaks in the Endicott Mountains include the
225:, the upper reaches of the West Fork of the
351:Natat Mountain at 5,141 feet (1,567 m)
305:Mount MacVicar at 6,693 feet (2,040 m)
302:Wichmann Tower at 6,916 feet (2,108 m)
229:(Kaluluktok Creek), Akabluak Pass, and the
342:Sirr Mountain at 5,712 feet (1,741 m)
339:Gray Mountain at 5,783 feet (1,763 m)
345:Frigid Crags at 5,501 feet (1,677 m)
323:Mount Stuver at 6,286 feet (1,916 m)
320:Iniakuk Peak at 6,490 feet (1,978 m)
292:Fan Mountain at 7,090 feet (2,161 m)
574:Mountains of Unorganized Borough, Alaska
482:
480:
478:
476:
119:70 mi (110 km) North-south
308:Ariel Peak at 6,685 feet (2,038 m)
111:151 mi (243 km) East-west
546:
381:sediments that have undergone partial
35:Endicott Mountains looking south, 1901
473:
295:Dan Peak at 7,055 feet (2,150 m)
286:Caliban at 7,181 feet (2,189 m)
391:Mississippian (early Carboniferous)
289:Xanadu at 7,160 feet (2,182 m)
13:
512:
14:
585:
531:
438:U.S. Geological Survey Bulletin
409:These peaks may all be found at
29:
518:Handschy, James William (1989)
415:United States Geological Survey
389:and continued through into the
463:
453:
443:
430:
420:
403:
1:
524:PhD Thesis, Rice University,
280:at 7,457 feet (2,273 m)
274:at 7,539 feet (2,298 m)
268:at 7,775 feet (2,370 m)
59:7,775 ft (2,370 m)
7:
10:
590:
362:
492:Geology of National Parks
257:, and highest to lowest:
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16:Mountain range in Alaska
87:68.33111°N 149.54694°W
538:"Endicott Mountains"
92:68.33111; -149.54694
540:from Peakbagger.com
172: /
83: /
440:1529-A, pp. Al-A64
272:Thibedeau Mountain
199:range of mountains
195:Endicott Mountains
176:68.367°N 152.300°W
41:Highest point
24:Endicott Mountains
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154:Range coordinates
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215:Dalton Highway
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554:Brooks Range
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239:Killik River
235:Alatna River
231:Noatak River
205:in northern
203:Brooks Range
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375:PreCambrian
369:crystalline
227:Kobuk River
223:Walker Lake
219:Atigun Pass
179: /
90: /
78:149°32′49″W
65:Coordinates
548:Categories
367:Above the
266:Mount Kiev
103:Dimensions
75:68°19′52″N
49:Mount Kiev
379:Paleozoic
124:Geography
55:Elevation
526:Abstract
496:page 380
387:Devonian
372:basement
237:and the
167:152°18′W
129:Location
490:(2004)
363:Geology
164:68°22′N
137:Country
502:
488:et al.
470:80–888
460:81–506
450:82–199
427:82–674
217:, and
213:, the
207:Alaska
197:are a
148:Alaska
145:Region
108:Length
397:Notes
249:Peaks
116:Width
500:ISBN
377:and
193:The
46:Peak
550::
498:,
475:^
241:.
417:.
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