Search results
Results from the WOW.Com Content Network
The central Colorado volcanic field (CCVF) is a volcanic field in Park County, Colorado.It is located in the southern Rocky Mountains and covered a roughly triangular area centered on the Thirtynine Mile volcanic area and extending from the Sawatch Range southeast to the northern Sangre de Cristo Range and the Wet Mountains and northeast to the southern Front Range south of Denver.
Geologic Map of the Central San Juan Caldera Cluster, Southwestern Colorado: Geologic Investigations Series. Vol. I-2799. U.S. Geological Survey "Central Colorado Volcanic field". Journal of Petrology. Archived from the original on 2013-01-13 "Central Colorado Volcanic field". Dr.
The Thirtynine Mile volcanic area, part of the larger Central Colorado volcanic field, is an extinct volcanic area located in Park and Teller counties, Colorado, northwest of Cripple Creek and southeast of South Park. [1] The area was the site of significant volcanism in the Paleogene Period about 35 million years ago.
Central Colorado volcanic field; S. San Juan volcanic field This page was last edited on 2 January 2016, at 18:52 (UTC). Text is available under the Creative Commons ...
San Juan volcanic field; Mount Sopris; South Table Mountain (Colorado) T. Tomichi Dome This page was last edited on 21 June 2021, at 00:32 (UTC). Text ...
Central Colorado volcanic field: Thirtynine Mile Mountain, elevation 11,553 ft (3,521 m), is a summit in the Front Range of the Pike National Forest in central Colorado.
Marshall Creek, Thirtynine Mile volcanic area, Central Colorado volcanic field; Colorado; 33.7 Ma; more than 100 cubic kilometres (24 cu mi) of Thorn Ranch Tuff. [8] [51] Mount Aetna (size: 10 km wide), Central Colorado volcanic field; Colorado; 33.81 Ma, 100 cubic kilometres (24 cu mi) of Badger Creek Tuff. [8] [52]
The lineament is defined by aligned volcanic fields and several calderas in the area, including the Valles Caldera National Preserve in the Jemez Mountains. The Jemez Lineament is thought to be a hydrous subduction zone scar, separating Precambrian basement rock of the Yavapai-Mazatzal transition zone from the Mazaztl Province proper.