Almost everything you see- not the little things, but the landscape at large across the whole planet.
But the obvious ones are fossils of oceanic organisms found in mountain ranges, mountains themselves- erosion should have caused them to flatten out over geological time scales yet there they are- process of uplift causes this.
Identical rock types and form on different continents shows they were once joined.
Evidence of glaciation includes their related landforms- moraines, u-shaped valleys, fjords and so on are still clear all over the UK and northern Europe and northern usa
Plate tectonics
The earths crust is a part of the outermost layer.
Silicon is a mixture of the minerals of the earths crust. so.... silicon isn't something from the earths crust. -thanks for your question.
thinner and denser
how wide is the earths crust
The presence of marine fossils in mountain rock
Yes, the crust is the top layer. It continually changes.
Compression is a force that changes Earth's crust by squeezing rock until it folds or breaks.
Contenintal Drift theory
Rock samples
Rock Samples.
Plate tectonics
Physical samples of rock extracted (taken) from deep within Earths crust.
Wave Length.
Physical samples of rock extracted (taken) from deep within Earths crust.
The earths crust is a part of the outermost layer.
Silicon is a mixture of the minerals of the earths crust. so.... silicon isn't something from the earths crust. -thanks for your question.