This post-assessment for Earth Science Regents focuses on rocks and minerals. It evaluates understanding of material hardness, mineral luster, density calculations, crystal formation, and composition of igneous rocks. Essential for students mastering geology fundamentals.
Fracture
Hardness
Streak
Luster
Cleavage
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1.0 g/cm3
2.0 g/cm3
5.0 g/cm3
10.0 g/cm3
20.0 g/cm3
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A
B
C
D
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Plagioclase feldspar, pyroxene, and olivine
Plagioclase feldspar, potassium feldspar, and quartz
Amphibole, calcite, and hematite
Amphibole, biotite mica, and gypsum
Biotite, Olivine, and pyroxine
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Rock 1
Rock 2
Rock 3
Rock 4
None of the rocks represented are metamorphic.
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Texture
Mineral Composition
Method of Formation
Crystal or Grain Size
Density
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The rock was formed by the metamorphism of sediments deposited in a terrestrial environment during the Cretaceous Period.
The rock was formed by the compaction and cementation of sediments deposited in a terrestrial environment during the Triassic Period.
The rock was formed from the solidification of magma in a marine environment during the Triassic Period.
The rock was formed by the metamorphism of sedimentary deposited in a terrestrial environment during the Triassic Period.
The rock was formed by the compaction and cementation of sediments deposited in a marine environment during the Cambrian Period.
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From clay and sand grain deposited, and cemented together by minerals
In Earth’s interior where temperatures exceeded the melting point of quartz
On Earth’s surface from the cooling of molten lava
In a desert when heat and metamorphic pressure caused quartz crystals to fuse together
Meteor impact from a large asteroid 65 million years ago
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0.0004 cm and less
0.0004 cm to 0.006 cm
0.006 cm to 0.2 cm
0.2 cm to 6.4
6.4 cm to 25.6
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