Midterm Study Guide 5 Flashcards

Rock Cycle

1
Q

What are the main distinctions for sedimentary rocks?

A
  • Composed of particles of previously existing rock (usually sandstone), these particles are not always homogeneous, however. stratification is visible. the presence of fossils. more porous and less dense than other rock types. react to dilute acids.
  • Clastic and Non Clastic
    - Clastic - Physical weathering and
    cementation or compaction to create
    rocks
    - Non-clastic - Chemical and biological
    weathering that later accretes into rocks
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Why are igneous rocks coarsely crystalline and extrusive ones finely?

A

Intrusive igneous rocks cool slowly, allowing their grains to form together, making them coarse. Extrusive igneous rocks are flash cooled, causing them to have small grains, making them fine.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

In which plate tectonic settings do you expect magma to form?

A

Environments include subduction zones, continental rift zones,[2] mid-ocean ridges and hot spots

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Why do melts migrate upward?

A
  • Melts move upward because they are less dense than the solids.
  • Less denser stuffs sink at the same time. the lighter ones go up.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

In which plate tectonic setting would you find regional metamorphism?

A

Continental

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

What are Steno’s laws?

A
  • Principle of Superposition: In a sequence of
    undisturbed layered rocks, the oldest rocks are
    on the bottom
  • Principle of Original Horizontality: Layered strata
    are deposited horizontally or nearly horizontally
    and nearly parallel to Earth’s surface
  • Principle of Lateral Continuity (cross cutting
    relationship): Layered rocks are deposited in
    continuous lateral contact
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

What are cross-cutting relationships?

A

States that the geologic feature that cuts another is the younger of the two features. Cross-cutting relations can be used to determine the relative ages of rock strata and other geological structures.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

sedimentary rock

A

made up of material derived from the breakdown of preexisting rocks. Rocks expose to water and air at the earth surface including chemical or physical break down, destroying some mineral and create new ones (ex: sand, clay and silt are compressed and become solid rock).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

mineral

A

the building blocks of rocks.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

intrusive

A

something occurring inside ex- intrusive igneous rocks

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

clay

A

compressed into shale

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

basalt

A

is a common extrusive igneous (volcanic) rock formed from the rapid cooling of basaltic lava exposed at or very near the surface of a planet or moon.

cools quickly

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

sandstone

A

is a clastic sedimentary rock composed mainly of sand-sized minerals or rock grains.
Most sandstone is composed of quartz and/or feldspar because these are the most common minerals in the Earth’s crust.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

foliation

A

repetitive layering in metamorphic rocks that can be thin or thick. (ex - mica)
schist

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

igneous rock

A

hot molten magma which erupted as volcanoes and associated lava flows on the earth’s surface, or as intrusive magma chamber which cooled far below the earth surface

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

metamorphic grade

A

(low-grade) shale -> slate -> schist -> gneiss (high-grade)

17
Q

grain size

A

grain size growth depends on the cooling time. Longer molten state means larger grains.

18
Q

pluton

A

intrusive igneous rock that is crystallized from magma slowly cooling. Cooled batholiths (large widespread magma chambers)..

19
Q

limestone

A

the most abundant non clastic sedimentary rocks, which precipitated from chemical solutions and/ or accumulated chemical, biological matter (crystalline, massive, skeletal)

20
Q

marble

A

metamorphic rock from limestone

21
Q

shale

A

the most abundant clastic rocks (compacted and cemented from detrital sediments)

22
Q

gneiss

A

(high grade metamorphic)

23
Q

metamorphic rock

A

has changed their form under influence of heat , pressure and fluid, preexisting rocks are modified to produce new one (differentiate from sedimentary rocks is change in the solid state, no melting)

24
Q

extrusive

A

formed above the earth’s surface

25
Q

continental shelf

A

the extended perimeter of each continent associated with a coastal plain. Submerged under relatively shallow seas. In the presence of a subduction zone next to an oceanic-continental convergence, there might not be a shelf.

26
Q

Decompression melting

A

A decrease in pressure, just as a rise in temperature, can melt materials, specifically rocks in this case. Therefore, decompression melting takes place as a result of less pressure being exerted on rocks. This occurrence is common at mid-ocean ridges where rocks are uplifted and consequently have less overburden.

27
Q

granite

A

Is a common type of intrusive, felsic, igneous rock which is granular and phaneritic in texture. This rock consists mainly of quartz, mica, and feldspar.

28
Q

diagenesis

A

physical/chemical processes of turning sediments into sedimentary rocks. Physical means: uses the process of lithification (compacting/cementing the sedments) to turn them to rocks.

29
Q

orogeny

A

process by which earth’s crust is folded and deformed by lateral compression to form a mountain range