

Sediment and Magma
Flashcard
•
Science
•
6th - 8th Grade
•
Hard
Barbara White
FREE Resource
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13 questions
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1.
FLASHCARD QUESTION
Front
Weathering Noun
[weth-er-ing]
Back
Weathering
The process where rock is broken down into smaller pieces called sediment by forces like wind and water.
Example: Weathering breaks down rocks into sediment layers, shown by the layers and sediment close-ups.
2.
FLASHCARD QUESTION
Front
Erosion Noun
[ih-roh-zhun]
Back
Erosion
The process by which sediment is transported from one location to another by natural forces like wind, water, or ice.
Example: Wind moves sand and dust, showing erosion by transporting sediment.
3.
FLASHCARD QUESTION
Front
Sediment Noun
[sed-uh-muhnt]
Back
Sediment
Small, solid pieces of material that are formed from the weathering of rocks and transported by erosion.
Example: Sediment layers form from weathered rocks, shown by different colored layers under water.
4.
FLASHCARD QUESTION
Front
Magma Noun
[mag-muh]
Back
Magma
Molten rock material located beneath the Earth's surface, formed when existing rock is melted by intense heat.
Example: A diagram showing a volcano with labeled parts, including the magma chamber beneath the surface.
5.
FLASHCARD QUESTION
Front
Compaction Noun
[kuhm-pak-shun]
Back
Compaction
The process where layers of sediment are squeezed and pressed together by the weight of the layers above them.
Example: Layers of sediment are squeezed together over time by the weight of the layers above them.
6.
FLASHCARD QUESTION
Front
Cementation Noun
[see-men-tay-shun]
Back
Cementation
The process where dissolved minerals crystallize and act as a natural glue, binding sediment particles together into solid rock.
Example: The image shows sediment layers with minerals acting as glue, binding particles into solid rock.
7.
FLASHCARD QUESTION
Front
Igneous Rock Noun
[ig-nee-uhs rok]
Back
Igneous Rock
A type of rock that is formed through the cooling and solidification of molten material like magma or lava.
Example: This diagram shows how igneous rocks form from cooling magma beneath Earth's surface.
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