Xenoliths are blocks of older rock enclosed in a body of younger igneous rock.
Older rocks that lie under younger rocks are called bedrock. Bedrock forms the solid foundation upon which younger rocks are deposited and can provide valuable information about the geologic history of an area.
Intrusions of igneous rock are typically younger than the rock layers they penetrate. This is because the magma that forms igneous intrusions is usually injected after the surrounding rocks have already solidified and formed.
The fault is younger than rock layer A. This is because faults are fractures in the Earth's crust that form after the deposition of rock layers, and activities like faulting can occur long after the rock layers have been deposited and solidified.
Dikes are always younger than the surrounding rock layers. The same holds true for any kind of intrusion. It will always be younger than anything that it is intruding into. To put it simply, you can't force an object into a bed of rock unless the bed of rock is already there.
You could tell an older rock from a younger rock by looking at it because the older rock isochron would have a steeper slope.
Xenoliths are blocks of older rock enclosed in a body of younger igneous rock.
Older rocks that lie under younger rocks are called bedrock. Bedrock forms the solid foundation upon which younger rocks are deposited and can provide valuable information about the geologic history of an area.
The law of superposition states: in horizontal rock layers, each layer is older than the one above it and younger than the one below it.
Intrusions of igneous rock are typically younger than the rock layers they penetrate. This is because the magma that forms igneous intrusions is usually injected after the surrounding rocks have already solidified and formed.
Extrusion is older than intrusion because, an extrusion is always younger than the rocks below it. An intrusion is always younger than the rock layers around and beneath it. Hope the answers correct ;)
Every layer of rock, as one moves up from the core, is younger than the one below it. This means that the layers of rock above and below the coal are different ages, with the one above younger and the one below older.
The layers of rock above the coal are younger, while the layers of rock below the coal are older. This is because sedimentary layers are deposited in a chronological sequence with the oldest rocks at the bottom and the youngest rocks at the top.
The layer of rock at the bottom of a sedimentary rock is older. This is due to the principle of superposition, which states that in an undisturbed sequence of rock layers, the oldest rocks are at the bottom and the youngest are at the top.
Principle stating that older rock layers are beneath younger rock layers.
The process of "overthrusting" occurs when tectonic forces push one rock layer on top of another, causing younger rock to be placed beneath older rock. This can lead to a reverse order of rock layers in a geologic formation. Another process, called "faulting," involves the movement of rock layers along a fault plane, which can result in the displacement of younger rocks below older rocks.
They measure how far away the rock is from the mid-ocean ridge. The farther, the older.