Earth's Layers
-Location of mountains and rock formations
-Same ancient climatic conditions on different continents
Focus: place WITHIN Earth along a fault at which the first motion of an earthquake occurs Epicenter: ON the surface, above focus, where seismic waves flow outward.
and caldera (basin-shaped depression).
Mantle: more magnesium, less aluminum and silicon (than crust)
Core: iron and nickel
-At transform boundaries -Caused by shear stress (pushes rock in parallel but opposite directions
-Mild eruptions -Lava (layers) builds cone
divergent: normal faults, shallow earthquakes convergent: reverse faults, strong earthquakes transorm: strike-slip, shallow earthquakes
-Form when rock is under tension (stress that stretches/pulls rock apart)
-Built by ash and lave pieces (cinders) that fall around vent
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-Forms during compression (stress that squeezes/pushes rock) -Hanging wall moves up relative to foot wall
-Large and steep -Formed by layers of hardened lava and pyroclastic materials -Mild eruptions