EARTH SCI Flashcards
happens when iron reacts with oxygen, leading to rust formation and the breakdown of rocks.
OXIDATION
a type of mechanical weathering, also called FROST ACTION, occurs when water enters cracks in rocks, treezes, expands, and causes the rocks to break apart.
FREEZING AND THAWING
Rocks that change due to pressure and heat are classified as
METAMORPHIC ROCKS
metamorphic rocks form around igneous intrusions under high temperatures and relatively low, uniform pressures.
NON-FOLIATED ROCKS
metamorphic rocks form around igneous intrusions under high temperatures and relatively low, uniform pressures.
NON-FOLIATED ROCKS
metamorphic rocks form under high, unequal pressures within Earth’s interior, where directed pressure dominates.
FOLIATED ROCKS
form from cooled magma or lava, derived from the Latin word “ignis,” meaning fire.
IGNEOUS ROCKS
form from cooled magma or lava, derived from the Latin word “ignis,” meaning fire.
IGNEOUS ROCKS
the internal heat retained from the early stages of Earth’s formation during its evolution.
PRIMORDIAL HEAT
generated from the decay of radioactive isotopes in Earth’s interior.
RADIOGENIC HEAT
the grinding of rocks by other rocks (correct), and halo-clasty refers to the formation of salt crystals which expand cracks in rocks after water evaporates.
ABRASION
involves upward movement of the earth’s mostly solid mantle
DECOMPRESSION MELTING
Magma can also be created when hot, liquid rock intrudes into the Earth’s crust. As the liquid rock solidifies, it loses this heat and transfer it to the surrounding crust.Repeated intrusions can transfer enough heat to increase the local geothermal gradient and cause melting of the surrounding rock and this creates a new magma
TRANSFER OF HEAT
occurs when water or carbon dioxide is added to rocks. The compounds cause the rock to melt at lower temperature
FLUX MELTING
occurs when water or carbon dioxide is added to rocks. The compounds cause the rock to melt at lower temperature
FLUX MELTING
consists of the continental shelf, slope, and rise.
THE CONTINENTAL MARGIN