everything from called to crystals is your predicate.
Seaside rock formations are sometimes called oolite.
The "sandwich" structure is due to the rock being from sediments deposited in sequential periods of activity and nature. Each single "slice" of solid rock is a "bed", and sequences of these build up "members" of "formations".
No. Intrusions are used to describe the process and resulting structure where igneous rocks force there way into or between pre-existing rock formations.
Those rock layers are quite colorful.
The formations that are sandwiched between layers of existing rock formations called sills. Another formation between layers is called laccoliths.
The formations that are sandwiched between layers of existing rock formations called sills. Another formation between layers is called laccoliths.
Wavy layers in rock deposits form due to folding, which occurs under high pressure and high temperatures. The rock layers bend and create the wavy appearance. Not sure if that is what you're looking for Wavy layers can also simply be a bedform within sedimentary rocks - these are called wavy bedding or wavy lamination.
Sills
Yes. This metamorphic rock can be made from granite; wavy bands of dark and light layers.
Disconformity.
Igneous rocks can disturb sedimentary rock layers and formations by their movement during ascent through such layer. when they make contact with this sedimentary rocks they could result to folding and/or metamorphism.
The wavy features found on some sandstones are the build up of the different layers of rock the rock has produced over the decades.
They are called Strata or Units, within Formations. I think the term "strata", which simply means "layers",is falling out of use for some reason.
everything from called to crystals is your predicate.
Seaside rock formations are sometimes called oolite.
The rock formations at the bottom are older.