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Coordinates: 44°58′27″N 113°26′42″W / 44.97417°N 113.44500°W / 44.97417; -113.44500
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<blockquote>We proceeded to the top of the dividing ridge from which I discovered immense ranges of high mountains still to the West of us with their tops partially covered in snow</blockquote> The next day Lewis met [[Cameahwait]] and his band of Shoshone, and returned with them across the pass to meet Clark. On August 26, 1805 the entire expedition crossed the pass.<ref>Ambrose, pp.269-282</ref>
<blockquote>We proceeded to the top of the dividing ridge from which I discovered immense ranges of high mountains still to the West of us with their tops partially covered in snow</blockquote> The next day Lewis met [[Cameahwait]] and his band of Shoshone, and returned with them across the pass to meet Clark. On August 26, 1805 the entire expedition crossed the pass.<ref>Ambrose, pp.269-282</ref>


In the early 19th century the pass was regularly used by the [[Blackfoot]] people, so that in 1824 [[Alexander Ross (fur trader)|Alexander Ross]] referred to the route as the Blackfoot route.<ref name="ishs280" /> At that time the pass itself was known as North Pass, to distinguish from [[South Pass (Wyoming)|South Pass]].<ref name="ishs280" /> The pass derives its present name from [[Fort Lemhi]], founded in 1855 by [[Mormon]] missionaries who were the first non-Indians to establish a sustained relationship with the [[Salmon River (Idaho)|Salmon River]] Indian people.
In the early 19th century the pass was regularly used by the [[Blackfoot]] people, so that in 1824 [[Alexander Ross (fur trader)|Alexander Ross]] referred to the route as the Blackfoot route.<ref name="ishs280" /> At that time the pass itself was known as North Pass, to distinguish it from [[South Pass (Wyoming)|South Pass]].<ref name="ishs280" /> The pass derives its present name from [[Fort Lemhi]], founded in 1855 by [[Mormon]] missionaries who were the first non-Indians to establish a sustained relationship with the [[Salmon River (Idaho)|Salmon River]] Indian people.


During the mining era the pass was used by stagecoaches, but the route fell into disuse after 1910, when the [[Gilmore and Pittsburgh Railroad]] was built through the nearby [[Bannock Pass]].<ref name="ishs280" /> Only a single track dirt road now crosses the pass.
During the mining era the pass was used by stagecoaches, but the route fell into disuse after 1910, when the [[Gilmore and Pittsburgh Railroad]] was built through the nearby [[Bannock Pass]].<ref name="ishs280" /> Only a single track dirt road now crosses the pass.

Revision as of 12:15, 21 February 2024

Lemhi Pass
View from Lemhi Pass
Elevation7,373 ft (2,247 m)
Traversed byUnpaved road
LocationLemhi County, Idaho / Beaverhead County, Montana,
 United States
RangeBitterroot Range of the Rocky Mountains
Coordinates44°58′27″N 113°26′42″W / 44.97417°N 113.44500°W / 44.97417; -113.44500
Lemhi Pass
Lemhi Pass is located in Idaho
Lemhi Pass
Lemhi Pass is located in the United States
Lemhi Pass
Nearest cityTendoy, Idaho
Coordinates44°58′27″N 113°26′42″W / 44.97417°N 113.44500°W / 44.97417; -113.44500
NRHP reference No.66000313
Significant dates
Added to NRHPOctober 15, 1966[1]
Designated NHLOctober 9, 1960[2]

Lemhi Pass is a high mountain pass in the Beaverhead Mountains, part of the Bitterroot Range in the Rocky Mountains and within Salmon-Challis National Forest. The pass lies on the Montana-Idaho border on the continental divide, at an elevation of 7,373 feet (2,247 m) above sea level. It is accessed via Lemhi Pass Road in Montana, and the Lewis and Clark Highway in Idaho, both gravel roads. Warm Springs Road, which roughly follows the divide in Montana, passes just west of the pass's high point.

History

The pass gained importance in the 18th century, when the Lemhi Shoshone acquired horses and used the route to travel between the two main parts of their homeland.[3] From the time of the Louisiana Purchase in 1803 until the Oregon Treaty in 1846 the pass marked the western border of the United States. On August 12, 1805 Meriwether Lewis and three other members of the Lewis and Clark Expedition crossed the Continental Divide at Lemhi Pass. Lewis found a "large and plain Indian road" over the pass.[4] This was the first time that white men had seen present-day Idaho:

We proceeded to the top of the dividing ridge from which I discovered immense ranges of high mountains still to the West of us with their tops partially covered in snow

The next day Lewis met Cameahwait and his band of Shoshone, and returned with them across the pass to meet Clark. On August 26, 1805 the entire expedition crossed the pass.[5]

In the early 19th century the pass was regularly used by the Blackfoot people, so that in 1824 Alexander Ross referred to the route as the Blackfoot route.[3] At that time the pass itself was known as North Pass, to distinguish it from South Pass.[3] The pass derives its present name from Fort Lemhi, founded in 1855 by Mormon missionaries who were the first non-Indians to establish a sustained relationship with the Salmon River Indian people.

During the mining era the pass was used by stagecoaches, but the route fell into disuse after 1910, when the Gilmore and Pittsburgh Railroad was built through the nearby Bannock Pass.[3] Only a single track dirt road now crosses the pass.

The pass was designated a National Historic Landmark in 1960.[2]

Mineral resources

The Lemhi Pass district has been found to host many lanthanide minerals and the richest deposit of thorium in the US. In a study of 31 samples taken from 21 different veins, the ratio of rare-earth elements (REEs) in the area is estimated to be between 0.05-9.2%. This depends largely on the localized mineralogy and REE mineralization. Most commonly the thorium is found as thorite hosted in quartz veins, whereas REEs are contained within monazite.[6]

The deposits lie within quartz veins hosted in Precambrian rock with minerals such as hematite, apatite, feldspar, thorite and monazite present. The monazite is found to be enriched in the middle rare earths, specifically neodymium (Nd), as there is estimated to be 35 weight percent of Nd in the monazite.[7] Neodymium, cerium, gadolinium, yttrium, and dysprosium are the top lanthanide minerals recorded to be attainable in the Lemhi Pass.[6]

See also

References

  1. ^ "National Register Information System". National Register of Historic Places. National Park Service. April 15, 2008.
  2. ^ a b "Lemhi Pass". National Historic Landmark summary listing. National Park Service. Archived from the original on January 10, 2008. Retrieved June 11, 2008.
  3. ^ a b c d Idaho State Historical Society Reference Series No. 280 Archived 2010-07-07 at the Wayback Machine
  4. ^ Ambrose, S.E. (1996) Undaunted Courage ISBN 0-684-82697-6 p.266
  5. ^ Ambrose, pp.269-282
  6. ^ a b Occurrence and Distribution of Rare Earths in the Lemhi Pass Thorium Veins, Idaho and Montana Mortimer H. Staatz, Van E. Shaw, and James S. Wahlberg (1972)
  7. ^ "Rare Earth Elements and Other Critical Metals in Idaho, Geo Note, Idaho Geological Survey, Virginia S. Gillerman, January 2011
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