Noun:

পাললিক শিলার স্তরভেদী গম্বুজাকৃতি আগ্নেয়শিলা,

laccolith's Usage Examples:

Carbon peak is a laccolith formed during the mid-Tertiary period, and is part of the “laccolith triangle” as described by the Colorado.

A laccolith is a sheet-like intrusion (or concordant pluton) that has been injected within or between layers of sedimentary rock (when the host rock is.

existing sedimentary rocks as the crown of a buried laccolith or possibly the underlying conduit of a laccolith.

Shonkin Sag laccolith, a famous laccolith 200 feet (61 m) thick and 1 mile (1.

A laccolith is an igneous.

West Beckwith Mountain is a laccolith, formed when magma intruded into Mancos Shale some 30 million years ago.

The Pine Valley Mountains form the Pine Valley Laccolith, one of the largest laccoliths in the United States.

The rocks of the buttes have been interpreted to be part of a laccolith, a magmatic stock or volcano conduits that became exposed at the surface.

Some of these intrusions form laccoliths emplaced at depths of a few kilometers.

range is made up of a yellowish granite underlain by grey gabbro-diorite laccolith and the sedimentary rocks it intrudes, deeply eroded by glaciers.

west of the mountain shows where the Eocene aplitic granite meets the laccolith top of the older Mesozoic granite ring dike.

Bear Butte is a geological laccolith feature located near Sturgis, South Dakota, United States, that was established as a State Park in 1961.

Carboniferous volcanic felsite (riebeckite), and may be the remains of a laccolith, a type of volcanic intrusion into the surrounding sedimentary rocks of.

A laccolith is a concordant intrusion with a flat base and domed roof.

The mountain is a laccolith.

suggests an impact crater; though it is actually the eroded remains of a laccolith.

intruded into the Mancos Shale resulting in a laccolith.

Given the fine-grained texture of the rock, the laccolith is assumed to have been at a shallow depth.

above a laccolith.

laccolith.

Each laccolith was fed by a radial dike at its distal end where it rolled over from vertical to form the horizontal laccolith.

The rock is a thick gabbroic-dolerite laccolith, which is a source of roadstone.