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LAYERS
accumulation between two surfaces
less sediment around the edges
diastromes between layers
diaclase go through multiple layers (velebit and dinarides)
FOLDS
deformation of layers with wave-like bending
subduction, side pressure, compression, elevation or lowering parts of continets
anticlines and sinclines
top of anticline is crest
axis plane goes through the crest downwards
FAULTS
parts of the lithosphere formed due to displacements of rocks
spreading, subduction, horizontal displacement of plates
medvednica, schwarzwald
TECTONIC RIDGE
formed by lowering parts of the crust along a fault
rhine valley, dead sea, eastafrican ditch
onlay (navlaka)
parts of the lithosphere where older layers cover the younger ones
result of compression in the orogeny stage of the formation of the crust
alps, gorski kotar, istra
EPIROGENIC MOVEMENTS
longterm movements of the crust which lead to faulting, folding and onlays
lowering makes oceans and seas, elevating makes land
regression (land↑ sea↓)
transgression (sea↑ land↓)
scandinavia, greenland, apeninski poluotok
netherlands, south china