Sujet

A group of 6 tent rocks at at the Kasha-Katuwe Tent Rocks National Monument

Légende

The Kasha-Katuwe Tent Rocks National Monument is a remarkable outdoor laboratory, offering an opportunity to observe, study, and experience the geologic processes that shape natural landscapes. The national monument, on the Pajarito Plateau in north-central New Mexico, includes a national recreation trail (see “Activities” below) and ranges from 5,570 feet to 6,760 feet above sea level. The cone-shaped tent rock formations are the products of volcanic eruptions that occurred 6 to 7 million years ago and left pumice, ash and tuff deposits over 1,000 feet thick. Tremendous explosions from the Jemez volcanic field spewed pyroclasts (rock fragments), while searing hot gases blasted down slopes in an incandescent avalanche called a “pyroclastic flow.” In close inspections of the arroyos, visitors will discover small, rounded, translucent obsidian (volcanic glass) fragments created by rapid cooling.

Info+

Photographe : Daniel Bayliss

Date

2007

Crédit

Photo12/Alamy/Daniel Bayliss

Notre référence

LMY20T04_B2W2X4

Utilisation

uniquement en France

Model release

Non

Property release

Non

Licence

Droits gérés

Format disponible

49,3Mo (1,8Mo) / 42,9cm x 28,8cm / 5072 x 3396 (300dpi)

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