Kasha-Katuwe Tent Rocks

New Mexico

Cone Heads

Kasha-Katuwe National Monument is located between Albuquerque and Santa Fe. This cluster of unique rocks was formed about 6.7-7 million years ago by two natural forces, namely, volcanic activities and erosion. Between volcanic eruptions, water and wind mixed the igneous materials with sand and gravel, generating different layers and colors of the rocks. The monument has a very interesting slot canyon. Although most parts of the trail is accessible, the last part is dangerous in winter because the slope is steep and icy.

Alex Yu, 2009

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