Sawtooth Mountain Range (Idaho)
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The Sawtooth Range is a mountain range of the Rocky Mountains in central Idaho, United States, reaching a maximum elevation of at the summit of Thompson Peak. It encompasses an area of spanning parts of Custer, Boise, Blaine, and Elmore counties, and is bordered to the east by the Sawtooth Valley. Much of the mountain range is within the Sawtooth Wilderness, part of the Sawtooth National Recreation Area and Sawtooth National Forest. The mountains were named for their jagged peaks.


Peaks

There are 57 peaks with an elevation over in the Sawtooth Range, all falling between on Thompson Peak, the highest point in the range. Another 77 peaks fall between . Climbs range in difficulty between the Observation Peak, a Class 1 hike, and King Spire, a rock route rated Class 5.10 on the Yosemite Decimal System.


Geology

The northern Sawtooth Range formed from the Eocene Sawtooth
batholith A batholith () is a large mass of intrusive igneous rock (also called plutonic rock), larger than in area, that forms from cooled magma deep in Earth's crust. Batholiths are almost always made mostly of felsic or intermediate rock types, such ...
, while south of Alturas Lake the mountains formed from the Cretaceous granodiorite of the
Idaho Batholith The Idaho Batholith is a granitic and granodioritic batholith of Cretaceous- Paleogene age that covers approximately of central Idaho and adjacent Montana. The batholith has two lobes that are separate from each other geographically and geo ...
. The Sawtooth Range has a history of alpine glaciation, but while no surface glaciers exist today, perennial snow fields and
rock glacier Rock glaciers are distinctive geomorphological landforms, consisting either of angular rock debris frozen in interstitial ice, former "true" glaciers overlain by a layer of talus, or something in-between. Rock glaciers are normally found at high ...
s remain, usually on north or east facing slopes. There have been 202 perennial snow fields mapped in the Sawtooth Range. The Sawtooth Range was last extensively glaciated in the Pleistocene, but glaciers probably existed during the
Little Ice Age The Little Ice Age (LIA) was a period of regional cooling, particularly pronounced in the North Atlantic region. It was not a true ice age of global extent. The term was introduced into scientific literature by François E. Matthes in 1939. Ma ...
, which ended around 1850 AD. Evidence of past glaciation given remnants of the glaciers such as glacial lakes, moraines, horns, hanging valleys, cirques, and arêtes.


Seismology

In 2010, scientists from Idaho State University discovered the Sawtooth Fault near the base of the mountains, running for near Stanley and Redfish Lake. The most recent large quakes along it occurred around 4,000 and 7,000 years ago. It is estimated the fault could produce a 7.5 magnitude earthquake, potentially felt as far as Boise.


Waterways

The Sawtooth Range is home to hundreds of lakes created by vanished alpine glaciers, with nearly 400 lakes in the Sawtooth Wilderness. Five of the six largest lakes in the range are located outside the wilderness ( Redfish,
Alturas Alturas (Spanish language, Spanish for "Heights"; Achumawi language, Achumawi: ''Kasalektawi'') is a city and the county seat of Modoc County, California. Located in the Shasta Cascade region of Northern California, the city had a population of ...
, Pettit, Yellow Belly, and Stanley lakes), while Sawtooth Lake is within the wilderness. Most of the east side of the Sawtooth Range is drained by the main stem of the Salmon River and the west side by the South Fork Payette River. Small portions of the northern and southern ends of the range are in the watersheds of the Middle Fork Salmon River and
Boise River The Boise River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. , accessed May 3, 2011 tributary of the Snake River in the Northwestern United States. It drains a rugged portion of the Sawtooth Range in sou ...
, respectively.


Recreation

There are 40 trails totaling nearly in the Sawtooth Wilderness that can be used for day hiking, backpacking, and horseback riding and accessed from 23 trailheads. Additional trails traverse the foothills of the mountains outside the designated wilderness. Camping is permitted anywhere in the wilderness. There are several developed campgrounds on the western side of range, outside the Sawtooth Wilderness, including at Redfish, Little Redfish, Alturas, Pettit, and Stanley lakes, as well as at Iron Creek. Restrictions on fires and animals apply in some areas.


See also

* Sawtooth National Recreation Area *
Lakes of the Sawtooth Mountains (Idaho) There are hundreds of lakes in the Sawtooth Mountains, most of which have been created by alpine glaciers. The majority of the lakes are within the Sawtooth Wilderness, but several are not yet still within Sawtooth National Recreation Area The ...
* Sawtooth National Forest * List of mountain ranges in Idaho * List of mountains of Idaho * List of mountain peaks of Idaho


References


External links


Sawtooth National Forest
- official website {{Authority control Ranges of the Rocky Mountains Mountain ranges of Idaho Salmon-Challis National Forest Sawtooth National Forest Sawtooth Wilderness Landforms of Custer County, Idaho Landforms of Boise County, Idaho Landforms of Elmore County, Idaho Landforms of Blaine County, Idaho