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The area has [[volcanic]] origins and is rich in [[potash]]. Many of the [[extrusive rocks]] and some of the [[dike]] rocks contain abundant [[phenocrysts]] of a clear [[analcime]] that appears to be primary. [[Leucite|Pseudoleucite]] is an abundant constituent of many of the [[igneous rocks]]. [http://www.minsocam.org/ammin/AM23/AM23_837.pdf]
The area has [[volcanic]] origins and is rich in [[potash]]. Many of the [[extrusive rocks]] and some of the [[dike]] rocks contain abundant [[phenocrysts]] of a clear [[analcime]] that appears to be primary. [[Leucite|Pseudoleucite]] is an abundant constituent of many of the [[igneous rocks]]. [http://www.minsocam.org/ammin/AM23/AM23_837.pdf]

{{coord missing|United States}}


[[Category:Mountain ranges of Montana]]
[[Category:Mountain ranges of Montana]]

Revision as of 21:26, 6 October 2008

The Highwood Mountains cover approximately 4,659 km² (1,799 sq mi) in north central Montana in the U.S., east of Great Falls and Benton Lake National Wildlife Refuge, at the northern end of the Lewis and Clark National Forest. [1] The mountains were included in Highwood Mountains National Forest until 1908, when the unit became part of Lewis and Clark National Forest.

Nearby are Highwood, Montana and the Missouri River above the mouth of the Marias River. The highest point in the Highwood Mountains is Highwood Baldy at 2338 meters (7670 ft). [2]

The area has volcanic origins and is rich in potash. Many of the extrusive rocks and some of the dike rocks contain abundant phenocrysts of a clear analcime that appears to be primary. Pseudoleucite is an abundant constituent of many of the igneous rocks. [3]