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had isolated radium from uranium ore, and she and her husband Pierre conducted research on radium and received the Nobel Prize for their studies in radioactivity. Ore from the Temple
Mountain mines was shipped to France for Madame Curie's radium experiments. There are accounts that she visited Temple
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zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and
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Mountain during one of her trips to the United States because she wanted to see where ore of such high quality originated. From 1948 through 1956, the Temple
Mountain area produced approximately 1,287,000 pounds of
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which is composed of the Church Rock, Moss Back, Monitor Butte, and Temple
Mountain Members. Uranium and other mined ore deposits are principally concentrated in the Moss Back Member. The oldest exposed rock is
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San
Raphael Reef WSA, Utah BLM Statewide Wilderness Draft Environmental Impact Statement, Volume VI, East-Central Region, page 13.
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383:, together forming the massive San Rafael Reef, which bounds the San Rafael Swell. Beneath these cliff-forming strata of the
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Mining claims were staked here as early as 1898, but no significant quantity of ore was produced until 1914 when mining for
340:, and prominently visible from long distances. It is situated approximately 45 miles (72 km) southwest of the town of
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began and continued intermittently into the 1920s. The Temple
Mountain mines were major uranium producers on the
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is a remote 6,820-foot (2,080 m) mountain and abandoned town, located on the southeast flank of the
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snowfall is generally light during the winter. Spring and fall are the most favorable seasons to visit.
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28:
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San Rafael
Secrets: What Did Madame Marie Curie Do in the Middle of a Utah Desert?
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Geology and
Uranium Deposits of the Temple Mountain District, Emery County, Utah
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Geology and
Uranium Deposits of the Temple Mountain District, Emery County, Utah
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Geology and
Uranium Deposits of the Temple Mountain District, Emery County, Utah
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The mountain was so named because the outline of this feature resembles the
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U.S. Geological Survey
Geographic Names Information System: Temple Mountain
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456:). During the uranium mining boom as a result of the escalation of the
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783:"Updated world map of the Köppen−Geiger climate classification"
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from this feature drains into Temple Wash which is part of the
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Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007).
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511:Temple Mountain, from the southwest, October 2015
499:Temple Mountain, from the southwest, October 2016
464:known as Temple City temporarily sprang up here.
371:This mountain consists of bleached, almost white
633:, published 13 April 2022, accessed 21 July 2022
767:The Emery County Archives and Dottie Grimes, "
754:C. C. Hawley, D. G. Wyant, and D. B. Brooks, "
728:The Emery County Archives and Dottie Grimes, "
715:C. C. Hawley, D. G. Wyant, and D. B. Brooks, "
693:C. C. Hawley, D. G. Wyant, and D. B. Brooks, "
344:, 7.9 miles (12.7 km) north-northeast of
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523:Temple Mountain, from the west, October 2009
423:in the late 1940s and early 1950s. Madame
33:Temple Mountain south aspect, October 2006
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745:", AuthorHouse Publishing, 2012, page 17.
476:system, Temple Mountain is located in a
885:Bureau of Land Management areas in Utah
758:", US Government Printing Office, 1965.
719:", US Government Printing Office, 1965.
697:", US Government Printing Office, 1965.
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387:are the lightly-colored slopes of the
16:Mountain in the American state of Utah
771:", Arcadia Publishing, 2008, page 96.
732:", Arcadia Publishing, 2008, page 89.
7:
657:Uranium Deposits of Temple Mountain
359:. Ownership is administered by the
188:Temple Mountain (the United States)
155:Location in Utah of Temple Mountain
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860:Landforms of Emery County, Utah
838:Temple Mountain rock climbing:
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880:North American 2000 m summits
603:"Temple Mountain - 6,820' UT"
474:Köppen climate classification
399:at the base of the mountain.
191:Show map of the United States
49:6,820 ft (2,080 m)
901:
444:, and 3,799,000 pounds of
107:38.6885833°N 110.6818250°W
79:8.6 mi (13.8 km)
808:10.5194/hess-11-1633-2007
566:List of mountains of Utah
379:, overlain and capped by
361:Bureau of Land Management
127:
69:Block Mountain (7,425 ft)
26:
834:National Weather Service
112:38.6885833; -110.6818250
59:840 ft (260 m)
787:Hydrol. Earth Syst. Sci
671:"Temple Mountain, Utah"
571:Uranium mining in Utah
478:Cold semi-arid climate
769:The San Rafael Swell
730:The San Rafael Swell
299:South-southeast Face
840:Mountainproject.com
799:2007HESS...11.1633P
741:Craig Evan Royce, "
653:Robeck, Raymond C.,
430:Triuranium octoxide
103: /
832:Weather forecast:
446:Vanadium pentoxide
397:Moenkopi Formation
39:Highest point
855:Mountains of Utah
472:According to the
440:), also known as
385:Glen Canyon Group
381:Kayenta Formation
373:Wingate Sandstone
320:, United States.
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875:Colorado Plateau
865:San Rafael Swell
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421:Colorado Plateau
389:Chinle Formation
346:Wild Horse Butte
330:Salt Lake Temple
310:San Rafael Swell
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230:Colorado Plateau
226:San Rafael Swell
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158:Show map of Utah
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625:Jensen, D. E.,
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544:Mountain portal
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610:. Retrieved
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314:Emery County
305:
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273:Type of rock
244:
220:Parent range
206:Emery County
793:(5): 1633.
558:Utah portal
462:shanty town
425:Marie Curie
354:Green River
342:Green River
324:Description
278:sedimentary
257:Age of rock
110: /
98:110°40′55″W
85:Coordinates
65:Parent peak
849:Categories
680:2020-11-24
612:2020-11-24
577:References
442:yellowcake
95:38°41′19″N
55:Prominence
817:1027-5606
123:Geography
75:Isolation
45:Elevation
530:See also
458:Cold War
413:vanadium
284:Climbing
266:Jurassic
262:Triassic
237:Topo map
202:Location
795:Bibcode
659:", 1954
485:Gallery
468:Climate
417:uranium
403:History
367:Geology
251:Geology
815:
415:, and
409:radium
350:runoff
813:ISSN
460:, a
318:Utah
242:USGS
210:Utah
803:doi
332:in
312:in
264:to
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811:.
801:.
791:11
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584:^
448:(V
432:(U
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363:.
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819:.
805::
797::
683:.
655:"
615:.
454:5
452:O
450:2
438:8
436:O
434:3
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
