Skip to main content
Advanced Search

Filters: Tags: Black Mesa (X)

3 results (163ms)   

View Results as: JSON ATOM CSV
Eolian deposition on the semiarid southern Colorado Plateau has been attributed to episodic aridity during the Quaternary Period. However, OSL ages from three topographically controlled (e.g. falling) dunes on Black Mesa in northeastern Arizona indicate that eolian sediments there were deposited in deep tributary valleys as early as 35–30 ka, with most sand deposited before 20 ka. In contrast, the oldest OSL ages for sand sheets fall within the Pleistocene-Holocene climatic transition (~ 12–8 ka). Thus most eolian sediment accumulated on Black Mesa under climatic conditions that were in general cooler, moister, and more variable than today, not more arid, pointing to a considerable increase in sediment supply....
thumbnail
This is a point coverage containing 12 years (1984 through 1995) of coal mining history in the Colorado Plateau coal assessment study area. This layer was derived from the Mine Safety and Health Administration's (MSHA) Information Resource Center data for the years 1984 through 1995.


    map background search result map search result map USGS 1:24000-scale Quadrangle for Black Mesa, NM 1996 Coal-mine production history from 1984 through 1995 in the Colorado Plateau coal assessment study area (cpmphg) USGS 1:24000-scale Quadrangle for Black Mesa, NM 1996 Coal-mine production history from 1984 through 1995 in the Colorado Plateau coal assessment study area (cpmphg)