Want this question answered?
An intrusion is a mass of igneous rock that forms when melted rock moves into cracks in rock layers and then cools.
A laccolith is an igneous formation between two sedimentary layers
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.
Older ; Younger . 1 (; N.R.C.J
Older rocks can be found above younger rocks in a cross section due to processes like faulting and folding. Faulting occurs when rock layers break and move along a fault plane, causing older rocks to be displaced above younger rocks. Folding occurs when rock layers are subjected to compressive forces, resulting in older rocks being pushed up and over younger rocks. These geologic forces create the observed order of rock layers in a cross section.
An intrusion is younger than its surrounding rock layers. An intrusion needs another rock to cut through it, which is referred to as a cross-cutting relationship.
younger over older is a phrase you can use to remember this principle.
The intrusion is younger than the overlying sedimentary rock.
It is younger than them.
It is younger.
It is younger.
An intrusion (:
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 ;)
Any igneous dike or intrusion is younger that the surrounding rock layers.
When you look at a rock that has undisturbed layers, the bottom layers are older and the upper layers are younger. Anytime a rock layer crosses another (ie. an intrusion), the crossing layer is younger.
(Intrusion) You can learn how old the rock layers are around it. the rock layers around under and all around the intrusion are always older than the intrusion itself. (EXTRUSION) the layers of rock bellow the extrusion is older than the extrusion.
An intrusion is a mass of igneous rock that forms when melted rock moves into cracks in rock layers and then cools.