MODULE 2: Minerals
ACTIVITIY/ASSESSMENT
Part I: Multiple Choice
B 1. Geologist who studies fossils is known as
a. seismologist b. paleontologist c. petrologist d. archeologist
D 2. The tendency of a crystallized mineral to break along certain directions yielding more
or less smooth, plane surface is ____.
a. fracture b. hardness c. tenacity d. cleavage
D 3. The tendency of a crystallized mineral to break along certain directions yielding more
or less smooth, plane surface is ____.
a. fracture b. hardness c. tenacity d. cleavage
C 4. Mineralogy Deals with
a. mode of occurrence
b. color of mineral
c. properties, formation and occurrence of minerals
d. types of minerals
C 5. It is a property of minerals that describes the ratio of the weight of the mineral by the
weight of an equal volume of water.
a. density b. unit weight c. specific gravity d. weight
C 6. It is term in geology as naturally occurring and coherent aggregate of one or more
minerals.
a. soil b. accessory minerals c. rock d. minerals
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Part II: Rate the following according to the Mohs Hardness Scale. 1 being the least hard to
10 being the most hard mineral.
MOHS HARDNESS
SCALE
Mineral Name Scale
Gypsum 2
Calcite 3
Apatite 5
Diamond 10
Topaz 8
Orthoclase 6
Quartz 7
Corundum 9
Fluorite 4
Talc 1
Part III:
Item 1 to 4: Four (4) Symmetry Elements of Crystals
Rotational symmetry
Mirror symmetry
Center of symmetry
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Roto inversion symmetry
Item 5 to 9: Four (4) physical properties of minerals
Streak
Hardness
Color
Luster
Item 10 to 14: Five (5) among several most common Rock forming Minerals
Quartz
Amphiboles
Micas
Olivine
Garnet
Glassy Texture Item 15: Sometimes called vitreous texture
Mineralogy Item 16: It is the study of minerals, their crystalline and chemical structures, and
their properties.
Mineral Item 17: A naturally occurring, inorganic, solid, crystalline substance which has a fixed
structure and a chemical composition which is either fixed or which may vary within certain
defined limits.
Crystallography Item 18: This refers to the experimental science of determining the arrangement
of atoms in crystalline solids.
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