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1
Minerals are ____ substances that are Naturally occurring in the environment
inorganic
2
Minerals are inorganic substances that are _____ in the environment
naturally occuring
3
They have a ___. They are composed of A Atoms Of certaiom Elements that are held together by Chemical bond
specific chemical composition
4
Molecules in a mineral are arranged in a repeated structure that form a _____^
solid crystal
5
The ___ of a mineral depends on the elemen which constitute the crystal lattice - the arrangement of atoms, or groups of atoms, in specific pattern and with high symmetry. The reflection of certain wavelengths of light by the crystal lattice results in the color perceived by the observer.
color
6
is the color of the mineral in its powdered form.
streak
7
___ is the measure of the resistance surface to abrasions or scratches.
hardness
8
Hardness is the measure of the resistance of a surface to abrasions or scratches. It is generally measured using ____
mohs scale of hardness
9
is the tendency of the mineral to be split or broken along flat surfaces
cleavage
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refers to the texture or shape of the mineral's surface when the mineral breaks into forms other than flat surfaces
fracture
11
is the relative differences in the opacity and transparency of a mineral as light is reflected on its surface. This describes the 'sparkles' of the mineral surfaces
luster
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Is the ratio of the weight of the mineral to the weight of the water with an equal volume. Phvsical Properties of Minerals
specific gravity
13
refers to the behavior of the mineral under deformation or stress such as cutting, crushing, bending, or hitting
tenacity
14
refers to the growth crystal pattern of a mineral as single or aggregated.
crystal habit
15
refers the ability of a substance to dissolve in a solvent at a specified temperature
solubility
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refers to the temperature at which solid turns into liquid. Minerals tomposed of atoms that are tightly bonded within the crystal structure have high melting points
melting point
17
has a chemical composition of SiO2. It is a glassy-looking hard substance with white streaks. Despite its hardness, with a Mohs hardness of 7, it is quite brittle. Pure quartz is clear and transparent. Colored varieties of quartz are due to elemental impurities built into its lattice. The grains of quartz, in general, are irregular in shape
quartz
18
has a chemical composition of XAl(1-2)Si(3-2)08, where X is K, Ca, or Na. It is quite hard with a Mohs hardness of 6. It is a light-colored material, usually white, but they can have lighter shades of red or green. It has a glassy luster. In rocks, feldspar forms rectangular crystals that break along flat faces
feldspar
19
is any group of hydrous potassium aluminum silicate minerals. The most common examples are clear muscovite and black biotite Mica is soft, with Mohs hardness ranging from 2 to 2.5. It is easily identified by its perfect cleavage, reducing it to thin smooth flakes. Its shine is responsible for the flashes of light in rocks such as granite and slate.
mica
20
minerals have a general composition of XY(AI,Si)206 where X is CaorMg and Y is either Mg,Fe,Al. Augite is the most common of this group. It has a glassy luster with streaks of white, light green, or light brown. It is generally black in color and has stubby prismatic crystals. Its key feature is its two cleavages at around 90°
pyroxene
21
has a dark color with a Mohs hardness ranging from s to 6, Hornblende is the most common amphibole, It has a glassy luster and an opaque characteristic Its crystals are very long and very thin
Amphibole
22
a silicate mineral with a general chemical composition of (Mg,Fe)2 SiO4, but calcium, manganese, and nickel can be substituted for magnesium and iron. It is known for its distinct olive-green color and commonly used in the gemstone industry as peridot. It is a glassy looking and transparent substance that is almost as hard as quartz. Its crystals have a granular shape.
Olivine
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formed from hardening and crystallization of magma or molten material that originates deep within the earth.
Igneous
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rocks that form when magma hardens beneath Earth's surface.
intrusive
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Intrusive called process
plutonic
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The slower the magma cools, the ___ the crystals
larger
27
When lava hardens on the Earth's surface.
extrusive
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Extrusive process called
volcanic
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Common visual properties of extrusive
small crystals vesicular texture no crystal at all
30
Texture of intrusive igneous rock
coarse grained
31
Texture of extrusive rock
fine grained
32
Coarse Grained - ____ cooling results in the formation of large crystals
slow
33
Fine Grained ⁃ ____ cooling of magma or lava results in rocks with small, interconnected mineral grains
rapid
34
⁃ ____ texture results from cooling that is so fast that minerals do not have a chance to crystallize.
glassy
35
- ___ texture (holes pores, or cavities) are the result of gas bubbles which often occurs during volcaníc eruptions.
vesicular
36
2 composition of igneous rock
felsic and mafic
37
- a lighter color - a lower density - rich in Silicon (Si) and Aluminum (All
felsic
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⁃ a darker color ⁃ a higher density -rich in Iron (Fe) and Magnesium (Mg)
mafic
39
1. by the deposition of the weathered remains of other rocks 2. by the deposition of the results of biologic activity 3. by precipitation from solution
sedimentary
40
- is a process that squeezes, or compacts, sediments
compaction
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• - is a process in which rocks are physically and chemically broken down by water air, and living things
weathering
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• - the process of land being raised to a higher level
uplift
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• - when an agent of erosion - water, wind, ice, or gravity - lose energy, it drops the sediments
deposition
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• - "glue" - takes place when dissolved minerals are deposited in the tiny spaces among sediments
cementation
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• - involves weathering and the removal of rock.
erosion
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-_composed of weathered bits of rocks and minerals
clastic sedimentary
47
Forms when dissolved n. precipitate from water solutions, (water usually evaporates or boils)
chemical sedimentary
48
Forms when shell fragments are cemented together or when plant remains are compacted into rock.
organically formed sedimentary
49
To change form
metamorphism
50
- Most changes occur at high temperatures and pressures a few km below the Earth's surface
metamorphic
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What causes metamorphism
heat and pressure
52
Metamorphic ___ hot magma moves intro rock making contact w/ existing rock
contact metamorphism
53
2 types of metamorphism
regional and contact
54
Metamorphic ____ Large amounts of pressure results in large-scale deformation and high-grade metamorphism (these rocks are very dense)
regional
55
2 types of regional metamorphism Pressure from ___ and ___
squished and plate movements
56
____ Metamorphic Rocks - rock has a layered or banded appearance.
foliated
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Notice_the _LIGHT dark LIGHT dark_layers
banded
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Crystals_appear squished_together
mineral alignment
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___ Metamorphic Rocks ⁃ ⁃ Does not have a banded texture. ⁃ Most only contain one mineral.
nonfoliated