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Chapter 6

Across
Small pieces of rock that are moved and deposited by water, wind, glaciers, and gravity
Rocks that are mainly composed of minerals that form with blocky crystal shapes
Occurs when very hot water reacts with rock, altering its mineralogy and chemistry
Process that affects large areas of Earth's crust, producing belts classified as low, medium, or high grade, depending on pressure on the rocks, temperature, and depth below the surface
Horizontal layering
Physical and chemical processes that transform sediments into sedimentary rocks
Formed as inclined layers of sediment are deposited across a horizontal surface
Down
The layers of chemical sedimentary rocks that form when concentrations of dissolved minerals in a body of water reach saturation due to the evaporation of water; crystal grains precipitate out of solution and settle to the bottom
Meaning broken
Bedding in which the particle sizes become progressively heavier and coarser toward the bottom layers
Most common sedimentary rocks; formed from abundant deposits of loose sediments that accumulate on Earth's surface
Local effect that occurs when molten rock meets solid rock
Occurs when mineral growth glues sediment grains together into solid rock
Percentage of open spaces between grains in a rock
Layers and bands of minerals in metamorphic rocks