Category
page 1Igneous intrusions
El Capitan
vertical rock formation in Yosemite Valley, California, United States
trap
formation of dark-colored, fine-grained, non-granitic intrusive or extrusive igneous rock
lopolith
thumb| Basic types of intrusions:
1. Laccolith
2. Small dike
3. [[Batholith
4. Dike
5. Sill
6. Volcanic neck, pipe
7. Lopolith
As a general rule, in contrast to the smoldering volcanic vent in the figure, these names refer to the fully cooled and usually millions-of-years-old rock formations, which are the result of the underground magmatic activity shown.]]
A lopolith is a large igneous intrusion which is lenticular in shape with a depressed central region. Lopoliths are generally concordant with the intruded strata with dike or funnel-shaped feeder bodies below the body. The term was first d
igneous intrusion
body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth
Kondyor massif
mountain
stock
geological feature
Slesse Mountain
mountain in British Columbia, Canada
Cathedral Peak
mountain in Yosemite National Park, California
Flute Summit
mountain in British Columbia, Canada
Sourland Mountain
mountain in the United States of America