she is a dike she has a lady for her love
It is called a dike.
A normal (but fairly massive) star.A normal (but fairly massive) star.A normal (but fairly massive) star.A normal (but fairly massive) star.
It is known as a dam or dam wall. Another structure would be a dike or a levee.
... more massive (it has more mass).... more massive (it has more mass).... more massive (it has more mass).... more massive (it has more mass).
dike
The two general shapes of intrusive igneous bodies are tabular and massive. Tabular bodies, such as dikes and sills, have a flat, sheet-like shape that forms parallel to the surrounding rock layers. Massive bodies, such as batholiths and stocks, are more irregular in shape and often form deep underground.
Batholiths are typically massive igneous rock formations that often extend over large areas. They are formed from the solidification of magma deep within the Earth's crust. While they may have tabular intrusions within them, the overall structure of a batholith is considered massive.
The magma that squeezes into vertical cracks between rocks and then hardens is called a dike. Dikes are tabular bodies of igneous rock that cut across the existing rock layers.
A vertical intrusion is a body of igneous rock that has forced its way up through the layers of pre-existing rock in a vertical orientation. These intrusions are known as dikes if they are relatively narrow and tabular in shape, or as volcanic necks if they are more massive and represent the remnants of ancient volcanic vents.
A dike is formed when lava cuts across rock layers and hardens. This igneous intrusion results in a narrow, tabular rock formation that can be exposed on the Earth's surface due to erosion or uplift.
A dike forms when magma is injected into a crack in the rock and solidifies underground. It is characterized by a tabular shape that cuts across existing rock layers. Dikes are typically composed of igneous rock, such as basalt or granite.
No, batholiths are not tabular. Batholiths are large, dome-shaped intrusive igneous rock formations that are typically composed of granitic rocks. They form deep underground through the solidification of magma and are commonly found in mountainous regions.
The feature formed when lava cuts across rock layers and hardens is called a dike. Dikes are tabular bodies of igneous rock that cut across the structure of the surrounding rock.
A dike is a tabular body of intrusive rock that cuts across pre-existing rock layers, while a vein deposit is a narrow, linear fracture filled with minerals that are precipitated from hydrothermal fluids. Dikes are igneous in origin, whereas vein deposits are often associated with hydrothermal mineralization.
How do I get a bigger dike
The address of the Dike Public Library is: 133 E Elder, Dike, 50624 0912