It's called a volcanic sill.
It is called a dike.
A sheet of igneous rock that protrudes into the surrounding layers of rock is called a dike. Dikes are most often horizontal sheets that can form in many layers.
It is called a dike.
Dikes: These are vertical or near-vertical sheet-like intrusions of magma that cut across existing rock layers. Laccoliths: These are dome-shaped intrusions of magma that push up overlying rock layers, forming a mushroom-like shape.
A dolerite dyke is a sheet-like igneous intrusion that cuts across the surrounding rock formations. It is composed mainly of medium-grained dolerite rock that solidified from magma that intruded into existing rock layers. Dolerite dikes are common in areas with volcanic activity or tectonic movement.
Hiatal hernia is a condition in which a portion of the stomach protrudes upward into the chest, through an opening in the diaphragm. The diaphragm is the sheet of muscle that separates the chest from the abdomen. It is used in breathing.
Clay minerals are sheet silicates, with a structure made up of stacked layers of interconnected silica tetrahedrons and alumina octahedrons. This sheet structure allows for water and other ions to be easily absorbed between the layers, giving clay minerals their unique properties.
A magma sill is a planar sheet of magma which is parallel to the surrounding rock.
A Sill is formed when a fluid rock (usually magma but it can be mud or salt) is squeezed in between the layers (usually horizontal) of older rocks before it solidifies in place. A Dike or Dyke is the opposite, here the fluid rock penetrates across the layering of the older rocks. Logically to get the material to form a Sill there must be an accompanying feeder Dyke.
most commercial bakeries sheet the dough, layer and fold 36 layers of dough, 18 layers of fat.
A tabular concordant intrusive structure refers to a type of igneous intrusion where the orientation of the intrusive body is parallel to the existing layering or structures in the surrounding rock. This results in the intrusion appearing as a tabular or sheet-like feature that runs parallel to the rock layers. The intrusive body is typically discordant to the sedimentary or metamorphic layers but its orientation is concordant.
The use of sandwiching multiple layers together, and also integrating plastic layers into this sandwich, then heating them to form a composite sheet.