cross-cutting relations (pan)

A rainbow unconformity in the Mojave Desert.

A canyon wall on west side of Panamint Valley in SE California –part of Death Valley National Park. (Image ID# pan-rainbowunconf)

Sawtooth Peak

Sawtooth Peak in California.

Sawtooth Peak (right) capped by Columbia River Basalt. Beneath it is granite of the Wallow Batholith –and off to the left, are the bedded rocks of the Martin Bridge Limestone. (Image ID# 140713-43s)

Sawtooth Peak, California

Sawtooth Peak in California.

Sawtooth Peak (right) capped by Columbia River Basalt. Beneath it is granite of the Wallowa Batholith –and off to the left, are the bedded rocks of the Martin Bridge Limestone. (Image ID# 140713-43e)

Mudcracks and Ripple Marks

Mudcracks and ripplemarks.

Mudcracks (left) and ripple marks (right) in rock of the Belt Supergroup. The mudcrack is about 20cm across; the ripple marks are roughly 1m across. (Image ID# belt-sedsrs-pic)

Cloudy Peaks

Clouds over St. Marys River.

Bright mountain peaks guard a quiet river. (Image ID# 140720-6)

Granite intruding Gneiss

Granite and gneiss in Rocky Mountain National Park.

1.4 billion year old granite intruding 1.7 billion year old gneiss. (Image ID# ig-23)

Marine Transgression diagram

Marine transgression

If you look at Time 1, you can see a coastline in cross-section, with sand being deposited closest to shore, mud a little farther out, and eventually carbonate material even farther out. As sea levels rise in Time 2, the sites of deposition for these materials migrates landward, putting mud deposition on top the earlier sand deposition and so on. In time 3, the sequence moves even farther landward, resulting in carbonate over mud over sand. If these materials become preserved and turned into rock, they form the sequence sandstone overlain by shale overlain by limestone – just what we see on top the Great Unconformity. (Image ID# transgression)

Great Unconformity in Wyoming

Great unconformity on the west side of the Teton Range in Wyoming.

The yellow arrow points to the contact between the Cambrian Sandstone and underlying Precambrian metamorphic rock. This area is called the Great Unconformity of Powell, named after it’s first observer John Wesley Powell in 1869. (Image ID# sru-14e)