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The texture of the gneiss indicates that the bedrock
conglomerate
travertine
coquina
kettle lake
nonsedimentary rocks originate in regions of great heat and/or pressure
dark bands, has a red color, and has a hardness of 7.0
potassium feldspar
underwent regional metamorphism
Which geologic feature is formed by this process?
conglomerate
travertine
coquina
kettle lake
nonsedimentary rocks originate in regions of great heat and/or pressure
dark bands, has a red color, and has a hardness of 7.0
potassium feldspar
underwent regional metamorphism
In the anorthositic gneiss, the mineral garnet is most likely observed in the
conglomerate
travertine
coquina
kettle lake
nonsedimentary rocks originate in regions of great heat and/or pressure
dark bands, has a red color, and has a hardness of 7.0
potassium feldspar
underwent regional metamorphism
Which limestone is classified as inorganic?
conglomerate
travertine
coquina
kettle lake
nonsedimentary rocks originate in regions of great heat and/or pressure
dark bands, has a red color, and has a hardness of 7.0
potassium feldspar
underwent regional metamorphism
A primary difference between sedimentary rocks and nonsedimentary rocks is that
conglomerate
travertine
coquina
kettle lake
nonsedimentary rocks originate in regions of great heat and/or pressure
dark bands, has a red color, and has a hardness of 7.0
potassium feldspar
underwent regional metamorphism
Which mineral has cleavage in two directions and is commonly used to manufacture ceramics?
conglomerate
travertine
coquina
kettle lake
nonsedimentary rocks originate in regions of great heat and/or pressure
dark bands, has a red color, and has a hardness of 7.0
potassium feldspar
underwent regional metamorphism
A mixture of rounded pebbles and sand was deposited in a river. Over time, these sediments were compacted and cemented together to form the sedimentary rock
conglomerate
travertine
coquina
kettle lake
nonsedimentary rocks originate in regions of great heat and/or pressure
dark bands, has a red color, and has a hardness of 7.0
potassium feldspar
underwent regional metamorphism
The photograph below shows one type of limestone described in the table. This type of limestone is best identified as
conglomerate
travertine
coquina
kettle lake
nonsedimentary rocks originate in regions of great heat and/or pressure
dark bands, has a red color, and has a hardness of 7.0
potassium feldspar
underwent regional metamorphism
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