Magma fills the gap between plates at DIVERGENT boundaries.
It forms an intrusion in the layer (An intrusion is liquid rock that forms under Earth, magma)
It's sill or batholith.
Sill
A dike.
If the magma forces itself along a plane that is parallel to the bedding or foliation planes of the rock strata then (in other words it squeezes between two existing layers) it is a sill. If however it cuts across the bedding or foliation planes it is a dyke. For more information, please see the related links.
A body of magma that cuts through (and across) adjacent rock. Similar to a secondary vent but it does not strike through the surface. It then hardens and forms rock. It is always younger than the rocks which surround it.
The sliping is between the covalently bonded layers in graphite - conventionally the bonding is assumed to be inter -molecular between the layers, principally London dispersion forces..
I'll answer it for you, since we both have the same book. & i'm always looking on my computer for answers.The five landforms created from lava and ash are:Volcanic Necks, Dikes, Sills, Batholiths, And dome mountains.1. Volcanic Necks- They form when magma hardens in a volcano's pipe.2. Dikes- Magma forces itself across rock layers and hardens.3. Sill- forms when magma squeezes between layers of rock.4. Popcorn- is a mass of rock formed when a large body of magma cools inside the crust.5. Dome Mountains- forms when rising magma is blocked by horizontal layers of rock.Hope i helped! :)
The phospholipid forms a bilayer (two layers).
The slab that forms when magma forces itself across rock layers is called a dike.
The slab of volcanic rock that is formed when magma forces itself across rock layers is called a dike. This will eventually build into mountains.
If the magma forces itself along a plane that is parallel to the bedding or foliation planes of the rock strata then (in other words it squeezes between two existing layers) it is a sill. If however it cuts across the bedding or foliation planes it is a dyke. For more information, please see the related links.
A dike.
feature a and b
In fractures that cut across rock layers
sill
sill
A body of magma that cuts through (and across) adjacent rock. Similar to a secondary vent but it does not strike through the surface. It then hardens and forms rock. It is always younger than the rocks which surround it.
A crosscutting feature is always younger than the rock layers it cuts through because the feature always forms after the rock layers have been formed, making the rock layers older.
Light itself, the way it plays across forms like architecture and landscape.
A crosscutting feature is always younger than the rock layers it cuts through because the feature always forms after the rock layers have been formed, making the rock layers older.