Chapter 20: Earth Materials 

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55 Terms

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Clast Size
________ also provides clues to help determine the depositional environment of the sediment that formed the detrital rock.
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Mineral
________: a naturally occurring element or compound that is inorganic, solid, and has a crystalline structure.
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Non-Silicate Groups
The ________ are a source of many valuable ore minerals and building materials.
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Minerals
________ can be classified using six basic crystal forms.
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Cementation
________: When minerals slowly precipitate out of water and fill spaces between clasts.
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Texture
________: describes the size, shape, and arrangement of the rocks.
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Silica
________ is a common term for a compound that contains silicon plus oxygen or silicon dioxide (SiO2)
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compaction
The process by which clasts stick together by being pushed together is called ________.
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Coal
________ usually develops from peat, a brown, lightweight deposit of moss and other plant matter.
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crystals
The types of atoms that are added depend on the atoms in the growing ________ surroundings.
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Fine
________- grained, extrusive igneous rocks often have grain sizes that are too small to be seen without magnification.
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atomic arrangement
The ________ and composition of minerals allow them to be sorted into groups.
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Sand
In order of decreasing size, clasts are classified as gravel, ________, silt, or clay.
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Metamorphic rocks
________ can be classified by their texture.
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Mechanical Weathering
________ occurs when physical forces break rocks into smaller clasts.
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Mineral crystals
________ can form in different ways.
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Bowens reaction series
The ________, shown below, illustrates the sequence in which minerals crystallize from magma at different temperatures.
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Inorganic
________ means that minerals are materials that are not produced by living organisms.
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Igneous
Any ________, sedimentary, or metamorphic rock can be changed through metamorphism.
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Feldspar
________ is an example of a mineral with two planes of cleavage.
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orderly internal arrangement of atoms
The ________ in a mineral often is related to its external crystal shape.
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Coarse
________- grained granite and fine- grained rhyolite both form from granitic magmas.
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Regional
________ and contact metamorphism cause changes that can occur over millions of years.
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Detrital Sedimentary Rock Composition
________ depends on sources of rock material that were eroded, transported, and eventually deposited.
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Mineral composition
________ is extremely variable, so adjectives are used to modify the general name of the rock.
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Clay Minerals
________, micas, and amphiboles are examples of minerals that contain water in their crystal structures.
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Sharp folds
________ sometimes display intense transformations in metamorphic rocks.
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Mineral Grains
________ are randomly oriented when no directed force is involved.
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Metamorphic Changes
________ in rocks are caused by thermal energy, pressure, and chemical reactions.
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Crust
The ________ is the outermost layer of Earth.
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Streak Test
A(n) ________ is performed by rubbing a mineral on an unglazed, white porcelain tile.
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Hardness
________: The physical property that measures resistance to scratching.
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Composition of Minerals
The ________ are indicated by their chemical formulas.
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Metamorphic Processes
________ produce rocks with different textures.
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Igneous Rocks
________ are those that form from molten magma.
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Metamorphic Textures
________ can also be nonfoliated where crystals are in more random orientations.
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Rock-Making Process
The ________ is a continuous cycle.
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Continental Material
It includes all ________ and the material that forms the ocean bottom.
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Mineral
a naturally occurring element or compound that is inorganic, solid, and has a crystalline structure
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Cleavage
The ability of a mineral to do this is the physical property
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Fracture
When a mineral breaks unevenly
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Hardness
The physical property that measures resistance to scratching
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Streak
The color of a mineral in powdered form
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Magma
Molten rock material found inside Earth
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Non
metallic minerals are valuable as well
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Rock
a naturally formed mixture containing minerals, rock fragments, or volcanic glass bound together
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Texture
describes the size, shape, and arrangement of the rocks
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Intrusive Igneous Rocks
form within, or push into, regions of Earths crust
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Extrusive Igneous Rocks
rocks that form from lava erupted at Earths surface
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Coarse-grained gabbro and fine
grained basalt both form from basaltic magmas
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Clasts
small bits and pieces
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Pore Space
The empty space between clasts
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Cementation
When minerals slowly precipitate out of water and fill spaces between clasts
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Foliated
crystals are arranged in layers and bands
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Rock Cycle
The continual changing of rocks into different types