The instructive feature that forms when magma is injected into fractures that cut across rock layers is called a "dike." Dikes are typically vertical or steeply inclined and can vary in thickness, often cooling quickly as they intrude into the surrounding rock. They are formed when magma forces its way into existing cracks, solidifying as it cools and creating a distinct geological feature.
They feature magma with very high silica content.
A concordant intrusive igneous feature like a sill can form when magma hardens between horizontal layers of rock. Sills are tabular bodies that are parallel to the surrounding rock layers.
A laccolith is an intrusive feature that may start as a sill but as more magma accumulates, it can cause the overlying rocks to bend and create a dome-like shape. Over time, this dome can grow larger and form a lens-shaped intrusion beneath the Earth's surface.
An igneous intrusive feature that forms from a lens-shaped mass of magma that arches the overlying strata upward is called a laccolith. Laccoliths typically create a dome-like structure as the magma pushes the surrounding rock layers upward. They are often associated with volcanic activity and can vary in size.
feature a and b
Rockbox
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is it faults??
ischial tuberosity
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They feature magma with very low viscosity
It must.
Spotlight
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id say faults the answer is faults