Reids Peak

{{Short description|Mountain summit in Utah, United States}}

{{Use mdy dates|date=January 2025}}

{{Infobox mountain

| name = Reids Peak

| photo = Reids Peak.jpg

| photo_caption = East aspect

| elevation_ft = 11724

| elevation_ref ={{cite web|url=https://listsofjohn.com/peak/18086|title=Reids Peak - 11,724' UT|website=listsofjohn.com|access-date=2024-06-09}}

| prominence_ft = 670.

| prominence_ref =

| isolation_mi = 0.59

| isolation_ref ={{cite peakbagger|pid=27798|name=Reids Peak, Utah|access-date=2024-06-09}}

| parent_peak = Bald Mountain (11,948 ft)

| etymology =

| map = Utah#USA

| map_caption = Location in Utah

| label_position = bottom

| map_size = 240

|part_type = Protected area | part =

| country = United States of America

| state = Utah

| region = Summit

| region_type = County

| coordinates = {{coord|40.7063807|N|110.9124702|W|type:mountain_region:US-UT_scale:100000_source:gnis|format=dms|display=inline,title}}

| coordinates_ref ={{cite gnis|id=1444862|name=Reids Peak|access-date=2024-06-09}}

| range = Uinta Mountains
Rocky Mountains

| rock = Quartz arenite

| age = Late Precambrian

| topo = USGS Mirror Lake

| first_ascent =

| easiest_route = {{YDS|2+}} scrambling

}}

Reids Peak is an {{convert|11724|ft|meter|adj=mid|-elevation|abbr=off|sp=us}} mountain summit in Summit County, Utah, United States.

Description

Reids Peak is located {{convert|50.|mi|km}} east of Salt Lake City in the Uinta-Wasatch-Cache National Forest. It is situated in the western Uinta Mountains which are a subrange of the Rocky Mountains. Precipitation runoff from this mountain drains north into headwaters of the Weber River. Topographic relief is significant as the summit rises {{convert|2300.|ft|m|abbr=off|sp=us}} above the Weber River in one mile (1.6 km). Access to the mountain is via the Mirror Lake Highway. The mountain was first named "Reeds Peak" in 1875, and the present spelling of the toponym was officially adopted in 1932 by the U.S. Board on Geographic Names. The peak is named after an early explorer of this region.[https://books.google.com/books?id=2IfBjJTQy6YC&dq=reids+peak+early+explorer+region+decisions&pg=RA3-PA24 United States Board on Geographic Names, Decisions of the United States Geographic Board], October 5, 1932, p. 24. William "Toopeechee" Reed was an early pioneer of this region who founded Reed Trading Post in 1828, making this the first permanent non-Indian residence and business in what would become the State of Utah.

Geology

Reids Peak is composed of metasedimentary rock of the Mount Watson Formation.[https://geology.utah.gov/potd-july-26-2016-wasatch-cache-national-forest-summit-county-utah/ Utah Geological Survey], Retrieved 2024-06-09. Fluvial sediment processes deposited a sequence of nearly white quartz arenite and subarkose interbedded with minor amounts of pale-red arkosic arenite and grayish-green shale during the Late Precambrian.[https://books.google.com/books?id=eivUcW8gn4oC&dq=mount+watson+formation+utah&pg=PA211 Gwendolyn W. Luttrell, Lexicon of New Formal Geologic Names of the United States 1981–1985], U.S. Geological Survey Bulletin, U.S. Government Printing Office, 1983, p. 211. The Uintas were uplifted during the Laramide orogeny about 70 to 50 million years ago. The area around Reids Peak and Bald Mountain became an ice cap during glaciation of the Ice age, transforming these peaks into nunataks.Wallace Walter Atwood, Glaciation of the Uinta and Wasatch Mountains, U.S. Government Printing Office, 1909, p. 12. Numerous glacial cycles during the Quaternary Period sculpted the peak and scoured the surrounding land forming many depressions that are now lakes. Viewed from the summit, as many as 70 lakes can be counted.[https://books.google.com/books?id=2s8aAQAAMAAJ&dq=Reids+Peak+uinta+70+lakes&pg=RA27-PA40 Commercial West, December 19, 1914], p. 40.

Climate

Based on the Köppen climate classification, Reids Peak is located in a subarctic climate zone with cold snowy winters and mild summers.{{cite journal | author = Peel, M. C. |author2=Finlayson, B. L. |author3=McMahon, T. A. |name-list-style=amp | year = 2007 | title = Updated world map of the Köppen−Geiger climate classification | journal = Hydrol. Earth Syst. Sci. | volume = 11 |issue=5 | pages = 1633–1644 |doi=10.5194/hess-11-1633-2007 |bibcode=2007HESS...11.1633P |s2cid=9654551 | issn = 1027-5606|doi-access=free }} Tundra climate characterizes the summit and highest slopes.

See also

Gallery

File:Reids Peak, Utah.jpg|North aspect of Reids Peak (center), with Bald Mountain (left). Kamas Lake in foreground.

File:Reids Peak se.jpg|Reids Peak viewed from the top of Bald Mountain.

File:Reids Peak ne.jpg|Northeast aspect

File:Reids Peak, Bald Mountain.jpg|Southwest aspects of Reids Peak (left) and Bald Mountain (right) viewed from Lost Lake

File:Reids Peak west.jpg|West aspect, from Reids Lake

References

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