Fossils
Both layers contain water.
Sedimentary rock can display strata, and some metamorphic rocks display metamorphic foliation; both can appear as stripes, layering, or banding.
Both oceanic and continental crusts consist primarily of igneous rock although they both contain some sedimentary rock. Oceanic crust is composed mainly of basaltic rock, while continental crust is composed of granitic rock.
Yes, they are and this is due to the fact that they are both intrusive (a rock having been forced between preexisting rocks or rock layers while in a molten or plastic condition).
It is most likely to be sedimentary. However both Igneous and metamorphic rocks can manifest a layered structure so this feature is not diagnostic on its own.
Both would have the same age, and according to plate tectonics, both Mexico and Australia would have been part of the same land mass.
Both layers contain water.
"Folding" is the term that describes the bending of rock layers due to stress.There are different types of Folds and these include:Anticlinal Folds: This is when the rock layers have an upward-arching folds.Synclinal Folds: This is when the rock layers have a downward, trough-like folds.Monoclinal Folds: This is when both rock layers ends are horizontal.
They are both layers of the Earth comprised of rock....other than that, there are no similarities.
Sedimentary rock can display strata, and some metamorphic rocks display metamorphic foliation; both can appear as stripes, layering, or banding.
Both were created under extreme heat and can contain crystals or gems.
Both igneous and metamorphic rock were created under extreme heat and can contain crystals or gems.
Dikes and sills are relatively thin. They both have magma to squeeze or force itself across layers of rock.
yes sedimentary rock countain all particles from both igneous and metamorphic rock.
Yes I think ************************************* If the fault is a fissure (crack) without any slippage (movement up or down) then the layers on both sides will remain on the same level. If slippage has occured, there will be no continuity of layers.
Both oceanic and continental crusts consist primarily of igneous rock although they both contain some sedimentary rock. Oceanic crust is composed mainly of basaltic rock, while continental crust is composed of granitic rock.
Dikes and sills are relatively thin. They both have magma to squeeze or force itself across layers of rock.