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Published bySucianty Sanjaya Modified over 5 years ago
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Basaltic – dense, dark- Colored igneous rock formed from magma
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Cementation – when sediments are glued “cemented” together
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Cleavage – physical property of some minerals that makes them break along smooth, flat surfaces
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Color – the hue, shade, or pigment of a mineral
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Compaction – when sedimentary rocks are compressed by the layers above them
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Extrusive – fine-grained igneous rock that forms when magma cools at or near earth’s surface
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Foliated – metamorphic rock which are folded and flattened into parallel layers
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Fracture – physical property of minerals that break with uneven, rough, or jagged surfaces
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Granitic – light-colored silica-rich igneous rock (less dense than basaltic)
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Hardness – measure of how easily a mineral can be scratched.
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Igneous – rock formed when magma or lava cools and hardens
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Intrusive – igneous rock with large crystals formed when magma cools below earth’s surface
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Lava – molten rock that flows from volcanoes onto earth’s surface
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Luster – the way a mineral reflects light (metallic or non-metallic)
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Metamorphic – forms from heat & pressure (changes a rock’s form &/or composition)
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Minerals – naturally occurring, inorganic solid w/definite chemical composition
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Moh – moh’s scale is used to measure the hardness of a mineral
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Nonfoliated – metamorphic rock where grains are rearranged but don’t form layers
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Rock – mixture of minerals, rock fragments, or organic matter
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Rock cycle – describes how rocks change slowly from one type to another
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Sedimentary – forms when sediments are compacted or cemented together into layers
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Sediments – loose rock fragments, mineral grains, and once-living plants & animals that have been eroded
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Streak – color of a mineral in its powdered form
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