Isopach and structure contour maps of the Burro Canyon(?) Formation in the Mesa Golondrina and Mesa de los Viejos areas, Chama Basin, New Mexico
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Abstract
In the Chama Basin a wequence of conglomerate, sandstone, and red, gray-green, and pale-purple mudstone occurs stratigraphically between the Upper Jurassic Morrison Formation and Upper Cretaceous Dakota Sandstone. This stratigraphic interval has been called the Burro Canyon Formation by several workers (Craig and others, 1959; Smith and others, 1961; Saucier, 1974). Although similarities in lithology and stratigraphic position exist between this unit and the Burro Canyon Formation in Colorado, no direct correlation has been made between the two. For this reason the unit in the Chama Basin is called the Burro Canyon(?) Formation.
Study Area
Publication type | Report |
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Publication Subtype | USGS Numbered Series |
Title | Isopach and structure contour maps of the Burro Canyon(?) Formation in the Mesa Golondrina and Mesa de los Viejos areas, Chama Basin, New Mexico |
Series title | Miscellaneous Field Studies Map |
Series number | 1496 |
Chapter | A |
DOI | 10.3133/mf1496A |
Year Published | 1983 |
Language | English |
Publisher | U.S. Geological Survey |
Publisher location | Reston, VA |
Description | 44.56 x 36.03 inches and 40.71 x 36.25 inches |
Country | United States |
State | New Mexico |
Other Geospatial | Mesa De Los Viejos, Mesa Golondria |
Scale | 24000 |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |