1st Semester Flashcards

(98 cards)

1
Q

This is considered the building blocks of rocks. It is crystalline solid, naturally occurring, involves inorganic processes, and is chemically specific.

A

Minerals

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2
Q

The presence and intensity of certain elements.

A

Color

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3
Q

The colors of minerals in powder form. This is distinctive for minerals and is used for identification.

A

Streak

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4
Q

It is the measure of its relative resistance to scratching, measured by scratching the mineral against another substance of known hardness on the Mohs Hardness Scale.

A

Hardness

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5
Q

It is used to describe how minerals break into pieces.

A

Cleavage and Fracture

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6
Q

This is when a mineral breaks into clean fragments, wherein the surface is flat.

A

Cleavage

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7
Q

This is when a mineral breaks in an irregular manner, wherein the surface is rough, uneven, or curved.

A

Fracture

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8
Q

Tells how a mineral’s crystals are arranged in crystal lattice.

A

Crystalline Structure

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9
Q

The symmetrical three-dimensional structural arrangements of atoms, ions or molecules inside a crystalline solid as points.

A

Crystalline Lattice

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10
Q

The degree to which light is transmitted through a mineral. Minerals can be opaque, translucent, or transparent.

A

Transparency or Diaphaneity

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11
Q

Indicates the ability of a mineral to attract or repel other minerals

A

Magnetism

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12
Q

Level of resistance or reaction of minerals to stress such as crushing, bending, breaking, or tearing

A

Tenacity

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13
Q

Measures the density of a mineral.

A

Specific Gravity

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14
Q

The way light interacts with the surface of a crystal, rock, or mineral

A

Luster

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15
Q

How do you identify silicate class minerals?

A

If it contains Si, O with some Al, Fe, Ca. Some examples are Olivine, Quartz, and Feldspar.

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16
Q

These minerals are mostly deposited in marine environments; areas with high rates of evaporation. Formed from dead bodies of marine organisms.

A

Carbonate Class

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17
Q

An icicle-shaped formation that hangs from the ceiling of a cave and is produced by precipitation of minerals from water dripping through the cave ceiling.

A

Stalactites

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18
Q

An upward-growing mound of mineral deposits that have precipitated from water dripping onto the floor of a cave. They grow from the cave floor.

A

Stalagmites

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19
Q

Common examples of Carbonate Class

A

Calcite, Malachite, and Azurite

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20
Q

Found where salty water slowly evaporates; areas with high evaporation rates.

A

Sulphate Class

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21
Q

Common examples of Sulphate Class

A

Barite, Celestite, and Gypsum

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22
Q

What are Halide class minerals used for?

A

Used in making fertilizer, rock salt, steel and aluminum.

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23
Q

These are rocks that form within the volcano.

A

Plutonic/Intrusive

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24
Q

Rocks that solidify outside the volcano.

A

Volcanic/Extrusive

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25
What happens when a rock rapidly cools?
The rocks are either glassy or fine grained. Crystals are much smaller but bigger in amount.
26
What happens when a rock slowly cools?
Results in the formation of large crystals, but fewer in amount.
27
Provide examples of extrusive rocks
Obsidian and Basalt
28
These type of rocks form when magma or molten rock cools and crystallizes.
Igneous rocks
29
The two types of Igneous Rocks
Extrusive and Intrusive
30
The two major groups of Silicates Minerals
Light Silicates and Dark Silicates
31
Rocks dark in color imply that they are
Low in Silica
32
Rocks light in color imply that they contain
High silica content
33
Basaltic rocks are _ in silica content
low
34
Andesitic rocks are _ in silica content
intermediate/or in the middle
35
Granitic rocks are _ in silica content
high
36
Ultramafic rocks are _ in silica content
extremely low
37
These are rocks made up of small individual minerals which can be distinguished through a microscope.
Aphanitic or Fine-grained
38
Rapid solidification leads to _
Fine grained or Aphanitic rocks
39
Slow solidification leads to _
Coarse grained or Phaneritic rocks
40
These are Igneous rocks with a distinct difference in the size of mineral crystals, with the larger crystals known as phenocrysts.
Porphyritic
41
Rocks with voids which represent gas bubbles.
Vesicular Texture
42
Rocks made up of small individual minerals which can be distinguished through a microscope.
Glassy Texture
43
What do vesicles in a rock imply?
It is an extrusive rock that underwent rapid cooling, preserving the gasses.
44
These are rocks with a mass of intergrown crystals that are roughly equal in size and large enough to be seen without a microscope.
Pyroclastic
45
What is Bowen's Reaction Series?
Bowen's reaction series answers the question as to how different rocks are formed from the same molten material. It involves magmatic differentiation.
46
The process of formation of sedimentary rocks in breaking down or dissolving of rocks and minerals on the surface of the earth.
Weathering or Erosion
47
This is where the process of weathering proceeds the products are carried off.
Transportation
48
The process of formation of sedimentary rocks where the layering down of sediment is carried by wind.
Deposition
49
These are rocks that are derived from sediments; unconsolidated fragments that have accumulated.
Sedimentary Rocks
50
A type of sedimentary rock formed from fragments of pre-existing rocks. These are either shells or bones.
Clastic
51
Sedimentary rocks with unlimited mass of cemented, roughly rounded pebbles, cobbles and boulder, clay, silt, or sand.
Conglomerate
52
Sedimentary rocks that consists of sand-sized particles.
Sandstone
53
A type of sedimentary rock that litrifty from the remains of organisms. (Flora and Fauna)
Organic
54
It is a type of rock that begins as sediments, which are then cemented together through natural processes.
Chemical
55
What is the process of formation of sedimentary rocks?
1. Weathering rocks 2. Transportation 3. Deposition 4. Compaction 5. Cementation
56
Metamorphic rocks vs. Sedimentary
Metamorphic rocks undergo changes in temperature and pressure. Sedimentary rocks undergo weathering and erosion.
56
What is a protolith?
A protolith is a parent rock.
57
What are metamorphic rocks?
Pre-existing rocks that change into new forms because of increases in temperature, pressure, and chemical fluids.
58
What are the two kinds of Metamorphism?
Contact and Regional
59
Define Contact metamorphism
- This happens when rock is heated up by an intrusion of hot magma. - Affects a small area
60
Define Regional metamorphism
- This happens along tectonic plates. - Regional metamorphism affects large volumes of rock - The pressure is rooted from the movement of plates
61
A texture in metamorphic rocks wherein it has many bindings. There is immense pressure that results in layered rocks. Mainly due to the pressure of regional metamorphism.
Foliated
62
A texture in metamorphic rocks that doesn’t have any layers or bindings. Mainly due to heat chrome contact metamorphism.
Non-Foliated
63
The earth’s crust broken into sections. Plates move around on the top of the mantle like rafts.
Lithospheric Plates
64
What makes the plates move?
Convection Currents in the mantle move the plates as the core heats the slowly-flowing asthenosphere.
65
This is the heat from the earth from the day it was created.
Primordial Heat
66
This is the heat coming from the spontaneous nuclear disintegration
Radiogenic Heat
67
Sources of heat transfer where heat energy is transmitted through collision of neighboring atoms/molecules, involving direct contact.
Conduction
68
Driven by temperature differences across fluid.
Convection
69
Energy that comes from a source and travels through space at the speed of light.
Radiation
70
The cause of tectonic plates in continuous motion.
Convection
71
The three kinds of plate boundaries
Divergent, Convergent, and Transform
72
A plate boundary where two plates separate. Pulled apart due to stress called tensional.
Divergent
73
What type of fault is formed in tensional stress?
A normal fault
74
What does a normal fault consist of?
A hanging wall and a foot wall.
75
What is the difference between a fault and a plate boundary?
A plate boundary is where two plates meet, whereas a Fault is a crack in a plate.
76
Provide the geologic features of Divergent Boundaries
1. Mid-ocean ridges 2. Rift valleys 3. Fissure Volcanoes
77
Collision or compressional stress of plate boundaries.
Convergent
78
A type of fault formed when the rock is squeezed from compressional stress.
Reverse Fault
79
What are the three types of Convergent Boundaries?
1. Oceanic-Continental 2. Oceanic-Oceanic Plate 3. Continental-Continental
80
Geologic features of Oceanic to Continental boundaries
Trenches and Subduction Zone
81
Geologic features of Oceanic to Oceanic boundaries
Trenches, Subduction Zone, Volcano, and a series of islands
82
Geologic features of Continental to Continental boundaries
Mountain Ranges
83
Geologic events of Oceanic to Continental boundaries
Volcanic Eruption and Subduction
84
Geologic events of Oceanic to Oceanic boundaries
Earthquake, Subduction, and Volcanic eruption
85
Geologic events of Continental to Continental boundaries
Earthquake
86
A plate boundary where two plates move past each other in opposite directions.
Transform Boundaries
87
What is the geologic event caused by Transform Boundaries?
Earthquake
88
A type of stress that acts coplanar with a cross section of material. This is when Rock is pushed in two opposite directions.
Shearing Stress
89
What happens next at Transform Boundaries?
May cause Earthquakes when the rock snaps from the pressure.
90
What happens when the rock is sheared or “cut” from the stress of shearing?
Strike Slip Faults are formed.
91
Natural history has been punctuated by catastrophic events that altered that way life developed and rocks were deposited. The Earth was formed by a series of catastrophes.
Principle of Catastrophism
92
The earth was shaped entirely by the operation (erosion, deposition, lifting) that acted over a long period of time (geological)
Principle of uniformitarianism
93
Technique to determine the age of a rock by comparing the historical remains to the nearby layers
Relative Dating
94
All rock layers are laterally continuous and may be broken up or displaced by later events.
Lateral Continuity
95
Any material that becomes trapped within a rock or mineral during its formation.
Inclusions
96
The geologic feature which cuts another the younger of the two features.
Cross-cutting relationship
97
A large plume of hot mantle material rising from deep within the Earth.
Hotspot