Unit 1 Flashcards

(161 cards)

0
Q

Physics

A

Helps understand rock structures and formations

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1
Q

Biology

A

Helps study and understand ancient biological organisms

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2
Q

Chemistry

A

Provides clues to geological material origins

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3
Q

Mathematics

A

Defines geologic processors quantitatively

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4
Q

Geology

A

Examine materials composing earth to help understand process that operate underneath us

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5
Q

What aspects of geology affect people (natural hazards)

A

Floods
Earthquakes
Volcanic eruptions
Landslides

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6
Q

Natural resources …

A
Oil and gas
Metals 
Coal, uranium 
Gravel , sand 
Water
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7
Q

What aspects of geology affect us in bc

A
Oil production -northeast bc/ off shre
Water use- water quality, agricultural use
Debris flows- Squamish highway 
Big earthquakes- vancouver
Rock quarries- Sumas mtn 
Floods- Fraser river 
Metals and pollution-Britannia mine
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8
Q

3 reasons y earth is hard to study

A

Processes occur slowly

2) earth is large
3) not predictable on local scale and human time

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9
Q

Catastrophism

A

Rock layers fossils granite etc. we’re produced during catastrophes such as volcanic eruptions

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10
Q

Static

A

Earth is quiet

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11
Q

The forefather to understanding modern geologic ideas was sir…

A

James Hutton

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12
Q

What theory did James Hutton develop

A

Principle of uniformitarianism

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13
Q

Principle of uniformitarianism

A

“The present is the key to the past” - geo processes we see today have operated thru time

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14
Q

Dynamic equilibrium

A

As internal forces push up, gravity and erosion are tearing down

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15
Q

How olds is the earth

A

4.5 bya

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16
Q

How does the earths age compare to the sun

A

Little younger

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17
Q

What does the Big Bang refer to

A

Start of the universe 14.5 bya

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18
Q

Where does the earths moon come from

A

Collisions spun off material = moon

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19
Q

What would early earth look like

A

Ball of rock

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20
Q

Solar nebula theory

A

Gas clouds condense into Sun and left over planets

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21
Q

What has spritzer been able to show us

A

Looks thru the dust and sees in infrared

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22
Q

When did out solar system begin forming

A

4.5 bya

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23
Q

Protostar

A

Dust and gas collapse in in itself and rotation increases, the centre of mass heats up due to friction

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24
What has to occur for an star to be born
Fusion
25
What elements are involved in making of a star
H+ + H+ ---> He2+
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The Big Bang is begging of what
The solar system universe
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How do heavier elements get created
Fusion
28
When a star blows up it is called....
Super nova
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What date to all meteorites date back to
4.5 bya
30
How do planets form in the remaining disc of dust and gas rotating around the sun
Charged particles attract in zero gravity
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When materials begun to collide together it is called
Acreation
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What brings most material together
Gravity
33
What would happen to gasses and ice at inner planet range
Evaporate
34
What type of material condenses at high temperatures
Metallic Mercury
35
What is earths nickname
Godly lox planet
36
How was early solar system different from today
20 planets rambling chaotically
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What is the theory of moons origin
Massive collision + reformation
38
2 differences in how igneous and sedimentary rocks form..
1) igneous from melt, sedimentary from solid | 2) igneous forms from melting of lava, sedimentary forms by lithification, weathering, transportation and deposition
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2 differences in how meta and igneous form
Metaphoric rocks are sedimentary rock morphed, igneous is from lava melt 2)igneous forms from cooling, meta from heat
40
Igneous ---> sediment
Uplift--> weathering--->erosion--->sediment
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Metamorphic---> igneous
Melt---> magma--> Cooling--->crystallization
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Sediment --> meta
Transport -->burial-->lithification --> sed-->heat/pressure--> recrystallize--> meta
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Magma to sediment via intrusive igneous
Cooling-->crystallization-->igneous--> uplift--> weathering -->sediment
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2 differences between intrusive and extrusive igneous
Intrusive is underground, extrusive above ground | 2) intrusive is slow, extrusive is fast
45
Isolated pool of seawater leaves a salt deposit when it evaporates
Sed
46
Lava erupts and solidifies under the ocean
Igneous
47
A limestone is heated and recrytallizes into marble
Morohic
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Magma underground cools and forms granite
Igneous
49
Calcium carbonate forms stalactites in a cave
Sed
50
Sandstone under a lava flow has recrystallized into quartzite
Morphic
51
What is the difference between a rock and mineral
Rocks contain minerals , minerals can not contain rocks
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Y do minerals have regular crystal form
External expression of internal arrangement
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Why is color unreliable
Inside may b different
54
What is streak
Minerals powdered form
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What is luster
Appearance of mineral
56
What is difference between cleavage and fracture
Cleavage is clean cut | Fracture is messy break
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Why does particular mineral cleave rather than break
Breaks along the weak points
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What shape fragment is produced when mineral has perfect cleavage
Cube
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What is come out conchodial fracture
Messy break ex. Bone breaking
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What is hardness of a mineral
Resistance of mineral to scratching
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Earths internal energy comes from 3 sources
Impact energy Gravitation energy Radio actually be decay
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Density of earth
Greater density toward the centre and less dense toward the surface
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Molten material is called
Magma
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Magma originates depths of
50-250 km
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When magma is released
Trapped gasses also release and is now termed lava
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Formed from lava at the surface are classified as
Volcanic rock
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Formed from magma at depth are termed
Plutonic rocks
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Volcanic rocks
Extrusive
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Plutonic rocks
Intrusive
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Magma consist of 3 components
Liquid portion called melt that is composed of mobile ions 2) solids are silicate minerals that have crystallized 3) volatiles which are gasses dissolved in melt (co2)
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Magma is not everywhere under the earth
It is produced from partial melting of rocks in crust and upper mantle
72
Heat comes from
Friction | 2) concentrated radio the be decay
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Geothermal gradient is
Increase of temp
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Role of pressure
Reducing pressure can cause melting
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Pressure reducing commonly occurs at
Divergent plate boundaries
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Role of volatiles where most common?
Subduction zones where ocean soaked crust is brought down into the mantle
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Addition of gases
Usually water that cause rocks to melt
78
Bowens reaction series
Minerals crystallize in a systematic fashion 2) during crystallization the composition of the liquid portion of the magma changes
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If a melt is low in silica and High in fe-mg
Mafic
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Silica rich and low in fe-mg
Felsic
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Felsic
Silica rich Light Lower gravity
82
Mafic
Silica poor Dark High gravity Ex. Olivine
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Coarse grained
Intrusive, big crystals, slow
84
Fine grained
Extrusive, small crystals, fast cooling
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What is a mineral
Naturally occurring, solid, inorganic, chemical make up of crystal structure
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What is a rock
Solid aggregate or mass of minerals
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Crystal form
External expression of the orderly internal arrangement | Ex. Halite
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Polymorph
Two or more minerals with the same chemistry but different crystal structure Ex. Diamond and graphite
89
Specific gravity
Does is feel heavier than average
90
Other special properties
Magnetism, reaction to acid, malleable, double refraction, taste, smell
91
Rock forming minerals are
Common minerals that make up most of earths crust
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How many minerals have been identified on earth
4000
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What are minerals grouped on
Chemistry
94
What is the most important and common minerals
Silicates (SiO)
95
Silicates
Compose of rock forming minerals | 2) very abundant due to large amounts of silicon and oxygen in crust
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The building block of all silicates
Silica tetrahedron
97
Silica tetrahedron
4 oxygen atoms surrounding a smaller silicon ion
98
Different structures that are created are
Single Chain Sheet Frame
99
Common silicate minerals
``` Olivine Pyroxene Amphibole Mica Feldspar Quartz ```
100
Clay
Result of weathering
101
Olivine
High temp & fe-mg , green , dark
102
Pyroxene
Single chain structure , 2 cleavages at 90
103
What is amphibole also known as
Hornblende - double chain structure
104
Mica
Sheets - one direction if cleavage - 2 types
105
Feldspar
2 directions of perfect cleavage
106
Quartz
Only silicate that is si & o - no cleavage
107
What are the most common minerals you will find in typical crustal rocks
Feldspar 51% Quartz 12% pyroxene 11%
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How much percent of earth is silicate
8%
109
Contain co3 React with acid Ex. Calcite
Carbonates
110
End in O | Ex. Hematite
Oxides
111
End in S | Ex. Galena
Sulfides
112
End in so4 | Ex. Gypsum
Sulfates
113
End in halogens F,cl ,br,I Ex. Halite
Halides
114
End in po3 | Ex apatite
Phosphates
115
Pure state minerals | Ex. Copper, diamonds
Native minerals
116
Fractional crystallization
Early formed crystals settle out of melt and are isolated from melt by crystals settling on top 2) mafic rocks form in bottom
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Assimilation
Meg a melts the surrounding country rock as pieces fall off and join the melt
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Magma mixing
Two melts combine to form intermediate composition between them
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Early formed crystals settle to the bottom of the melt and are isolated from the rest of the melt ...
Fractional crystallization
120
Could fractional crystallization cause initial Felix turn to magic
No, order on how crystals form and first stable crystals that form are mafic. 1500------------->600 cannot jump
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Igneous rocks are classified on
Texture and minerals
122
Factors that affect crystal size are mostly due to
Rate of cooling
123
Slow rate
Fewer but larger crystals
124
Fast rate
Many small crystals
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Very fast
Glass
126
Texture
Appearance of rock
127
Fine grained
Aphanite
128
Coarse grained
Phaneritic
129
Extremely fast cooling
Glassy texture
130
With no gas escaping the rock formed is termed
Obsidian
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Gas escaping and creating frothing the rock is termed
Pumice
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Large crystals surrounded by a matrix of smaller crystals
Porphyritic
133
Reasons of porphyritic
Minerals form at different temperatures
134
Huge coarse grained crystals
Pegmatitic
135
Escaping gas leaving holes in the rock is called
Vesicular
136
Fragments from volcanic eruptions encased in rock is called
Pyro clastic
137
Rock containing large pieces of pyro clastic
Breccia
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Rock containing just ash
Tuff
139
Once magma cools and solidifies underground the general term for this feature is called
Pluton
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Shape of plugins can be
Tabular or massive
141
Surrounding rock is
Country rock
142
Concordant
Parallel to country rock
143
Discordant
Cut across the country rock
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Batholith
- largest, 100 km diameter, forms core of mountains - high viscosity magma(slurpy),rises slowly, rising melts crust and push into dome - silic , discordant
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Stock
- same as batholic but smaller - silic - discordant
146
Senility
Pieces of country rock that been detached - mafic,inter,silic - foreign rock - 1cm-->20m in size
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Chilled margins
Smaller crystals at edges where in contact with country rock - outside cool faster than inside - mafic,inter,silic
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Sill
``` Sheet like, along grain of country rock -usually horizontal -1m-->100m -low viscosity, squirty, mafic Concordat ```
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Dyke
Sheet like crosses the bedding of country rock - same as sill - intermediate - low viscosity - discordant
150
Laccoliths
- curved top with flat bottom - began as a sill but unable to extend laterally and created dome - medium viscosity , intermediate - concordat
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Viscosity
Resistant to flow
152
Mafic
Rich in ferromagnesian minerals, flows easily, low viscosity, gasses release easier resulting in non explosive eruptions
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Felsic
High in silica content , difficult to flow, Hugh viscosity, explosive Volpcanism
154
Composite volcano (strato)
``` 20km wide 5km high Slope 20-30 degrees (steep) Made of lava and pyroclastics High viscosity keeps sides steep Silic and inter Ex.cascade,rainier,Helens,baker ```
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Volcanic dome
``` 1km width 300m high 30-40 angle slope Very slow extrusion of very high viscosity lava Ex Helens Felic ```
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Volcanic pipes and necks
Pipes-connect magma to surface | Necks-resistant vents left standing after erosion has removed volcanic cone
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Shield volcano
``` Like a shield 5-10 angle Non explosive Large area Mafic Low viscosity Basalt Ex. Maura Loa ```
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Cinder cones
``` Built from ejected lava Occur in groups Small size Semi explosive Distinct look ```
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Fissure eruptions
Lava plateau Lava from cracks Mafic Low viscosity
160
Caldera
Massive explosiveness Eruption that results in a lake Felix High viscosity