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2.1 REVIEW

Teacher: Mrs. Dallimore
Horizontales
Organic matter in soil
Type of boundary when two plates move apart
Soil texture with smallest particle size
Formed by Weathering, erosion, deposition, compaction, cementation
Movement of either sudden or creeping large amounts of earth material caused by heavy rains that loosen materials on a slope and are then pulled downward by gravity
Type of boundary when one continental plate and one oceanic plate converge
Physical breaking apart of rock caused by wind, water, ice, and gravity
Layer that is composed of the earth's crust and the upper mantle
Type of boundary when two continental plates converge, Himalayas are an example
Water, wind, ice, and gravity
Soil texture with moderate particle size
Uprising of magma through cracks in the earth's crust caused by the interaction of tectonic plates, may be predicted by animal movement and ground swelling
Caused by gravity acting on an over-steepened slope
Massive amounts of snow and ice which move due to gravity
Verticales
Water, air, mineral matter, organic matter
How rocks change type over time with the power of the sun and the heat of the Earth's interior.
Type of boundary when two plates slide past one another, San Andres Fault is an example.
Changing of rock minerals may be caused by water and heat
Liquid layer made up of the mid-mantle beneath the lithosphere
Formed by pressure and high temperatures
Forms when magma cools and hardens
Indicates the magnitude of an earthquake
Vibrations of the Earth caused by the interaction of tectonic plates
Organic and mineral matter that make up Horizons O and A
The place where movement first occurs that causes an earthquake
Soil texture with largest particle size