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Mount Blanco
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Mount Blanco is a small white mesa — an erosional remnant — located on the eastern border of the Llano Estacado within Blanco Canyon in Crosby County, Texas. Blanco Canyon is a drainage channel carved into the Llano Estacado by the White River, a tributary of the Brazos River.
image:Mt_Blanco_1891.jpg|Early photo of Mount Blanco (1891)
image:Mount Blanco 2002.jpg|More recent photo of Mount Blanco viewed from south (2002)
image:Mt_Blanco_2005.jpg|Mount Blanco viewed from above (2005)
image:Blanco Formation Road Cut.jpg|Blanco and Blackwater Draw formations are exposed at this road cut along Texas Ranch Road 193.

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Encyclopedia
Mount Blanco is a small white mesa — an erosional remnant — located on the eastern border of the Llano Estacado within Blanco Canyon in Crosby County, Texas. Blanco Canyon is a drainage channel carved into the Llano Estacado by the White River, a tributary of the Brazos River.
image:Mt_Blanco_1891.jpg|Early photo of Mount Blanco (1891)
image:Mount Blanco 2002.jpg|More recent photo of Mount Blanco viewed from south (2002)
image:Mt_Blanco_2005.jpg|Mount Blanco viewed from above (2005)
image:Blanco Formation Road Cut.jpg|Blanco and Blackwater Draw formations are exposed at this road cut along Texas Ranch Road 193. (2002)
Geology The term "Blanco beds" was first applied to this formation in 1892 by William F. Cummins of the Geological Survey of Texas. The Blanco beds are considered to be of lacustrine origin – deposited in a Pleistocene lake basin set in the Ogallala formation of Pliocene age which underlies the upper surface sediments of the Llano Estacado. The thickness of the Blanco beds varies from around 22 to 26 m thick at the most. The formation mainly consists of light-gray fine-grained mudstone, sandstone, and some conglomerate. These light-colored sediments contrast sharply with the rust-colored sediments of the Ogallala Formation.
Mount Blanco is the type locality of the Blanco Formation and Blancan Fauna, which occurs throughout North America.
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