The in-place granular disintegration product of granite is called

Study for the ASBOG Fundamentals of Geology exam. Access flashcards, multiple-choice questions, and understand key geologic principles. Prepare confidently for your exam!

Multiple Choice

The in-place granular disintegration product of granite is called

Explanation:
Granite exposed to weathering breaks down mechanically into a loose, gritty, sandy-muddy mass that remains in place at the surface. This in-place granular disintegration product is called grus. It’s the weathered, in-situ material you’d find at the ground surface before further alteration to saprolite or soil or before any transport away as scree or alluvium. Quartz sand would be isolated quartz grains, not the specific in-place product of granite weathering; sandstone is a cemented sedimentary rock formed from deposited sand grains; gravel consists of larger rock fragments that have been transported and deposited. The term grus uniquely describes the granular, in-situ product of granite weathering.

Granite exposed to weathering breaks down mechanically into a loose, gritty, sandy-muddy mass that remains in place at the surface. This in-place granular disintegration product is called grus. It’s the weathered, in-situ material you’d find at the ground surface before further alteration to saprolite or soil or before any transport away as scree or alluvium.

Quartz sand would be isolated quartz grains, not the specific in-place product of granite weathering; sandstone is a cemented sedimentary rock formed from deposited sand grains; gravel consists of larger rock fragments that have been transported and deposited. The term grus uniquely describes the granular, in-situ product of granite weathering.

Subscribe

Get the latest from Passetra

You can unsubscribe at any time. Read our privacy policy