These columnar basalts near Mammoth Lakes in California are comparatively recent, about 100,000 years old, but are part of a long lived sequence of volcanic events resulting from subduction beneath the west coast of north America. The Sierra Nevada was uplifted and metamorphosed about 140 million years ago by the subduction, that melted the crust and formed the granites of the mountain range.
Volcanism restarted around 30 million years ago, and its remnants litter the landscape of the west of the continent as the second incarnation of the Sierras was uplifted, and their rise accelerated about 2 million years ago. The mountains were eroded by glaciers during the sequence of ice ages that began around that time and ended around 10,000 years back, creating a series of U shaped valleys. The interacting forces of volcanism, uplift and glacial erosion created the range we know today.
The Postpile began as a 120 meter deep basaltic lava lake that spewed from a vent some km northwards of the monument and it flowed down the river valley until it was dammed, probably by a glacial moraine. As it cooled and crystallised the rock shrank and cracked due to internal stress into the hexagonal forms that form this cliff. Due to its great thickness, the lake cooled slowly and evenly, resulting in the long (up to 20 metres) and symmetrical columns. The original rock formation was much taller, further glaciations have excavated the rock and planed off the top leaving striations caused by rocks embedded in the ice, while freeze thaw erosion has split off many columns, visible in the talus slope below.
It was declared a national monument in 1911after lobbying by John Muir when proposals were made to blast it in order to install a hydroelectric dam on the San Joaquin river.
Image credit: Peretz Partensky.
http://www.visitmammoth.com/things-to-do/summer-activities/devils-postpile/ http://www.nationalparks.org/explore-parks/devils-postpile-national-monument http://www.nps.gov/depo/naturescience/geology.htm