rocks Flashcards

1
Q

types of rocks

A

Igneous
Sedimentary
Metamorphic

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

rock cycle

A

All rocks on Earth are locked into a system of cycling and re-cycling.

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

Sedimentary rocks

A

Rocks that are formed from erosion, deposition, and cementation.

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

Igneous

A

rocks that are formed from melting and cooling

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

Metamorphic

A

rocks that are formed by changing temperature and pressure

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

Intrusive Igneous rocks

A

Slow cooling deep beneath the Earth’s surface allows crystals to grow to a large size (1/8” or more). These crystals are easily visible

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Extrusive Igneous rocks

A

Rapid cooling near or at the Earth’s surface produces many small crystals that are not readily seen by the unaided eye. Typically volcanic in origin, and Cooling may be so rapid that crystals do not have a chance to form and instead a glass is produced.

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

Granite

A

a coarse to medium-grained rock that forms from the cooling of magma deep within the Earth (intrusive). It is made up mainly of varying amounts of the minerals: quartz, orthoclase, muscovite, biotite and hornblende. The name is from the Latin granum, for “grains”.

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

PEGMATITES

A

classified as intrusive igneous rocks, but there is a difference. They are VERY coarse grained and strictly speaking are not crystallizing out of a magma.

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

Diorite

A

very similar to granite, but is distinguished in the hand specimen by the absence of visible quartz.

Generally it has a salt and pepper appearance

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

Gabbro

A

a coarse-grained rock that is high is iron & magnesium-bearing minerals (pyroxenes, amphiboles, plagioclase feldspar, olivene). The rocks will be dark in color, somewhat heavier than granitic rocks and devoid of quartz.

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

Peridotite

A

or DUNITE is composed of 90-100% olivine. As a result it is characteristically olive-greens in color.

This material is thought to have originated in the upper mantle of the Earth.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

RHYOLITE

A

name comes from the Greek rhyo, from rhyax, “stream of lava”. It is formed when molten rock with the same composition as a high silica granite oozes to the Earth’s surface; and therefore cools quickly so only microscopic-

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

ANDESITE

A

is the fine-grained equivalent of DIORITE. It tends to be a darker gray than rhyolite and is often porphyritic, with visible hornblende.

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

BASALT

A

occurs as thin to massive lava. flows, sometimes accumulating to thicknesses of thousands of feet and covering thousands of square miles.

dark, fine-grained and often vesicular (having gas pockets). The pockets may be filled with secondary minerals

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

Pahoehoe (basalt)

A

a feature that forms on the surface of very fluid basalt flows. Much like the skin on a bowl of tomato soup – the surface in contact with the air begins to crystallize, while the fluid lava below continues to flow. This drags the upper, still plastic, surface into a series of smooth wrinkles.

17
Q

OBSIDIAN

A

volcanic glass (an acrystalline “solid” –actually a supercooled liquid). Its glassy, lustrous and sometimes banded appearance makes it rather easy to distinguish from all other rocks.

18
Q

PERLITE

A

is a light gray volcanic glass, having numerous concentric cracks which give rise to a perlitic or onion skin structure. It is generally of rhyolitic composition. It also exhibits a pearly luster.

19
Q

PUMICE

A
highly vesicular (i.e. it has lots of gas bubble holes) and is of rhyolitic composition.
Due to the many small holes, it is lightweight and will often float in water.
20
Q

Tuff

A

the accumulation of ash and small pyroclastic debris. Thick beds may form for many miles around a very explosive volcano, such as Mt. St. Helens.
Often, when the material is still hot upon deposition, it welds into a very hard rock.

21
Q

Volcanic Breccia

A
is pyroclastic (fire-formed fragments) and forms in explosive eruptions.  It is a mix of large angular fragments and small ash.
Often, the material is hot when it comes to rest and cools (welds) into a very hard rock.
22
Q

CLASTIC

A

sedimentary rocks that are composed of particles of pre-existing rocks

23
Q

CHEMICAL/BIOCHEMICAL

A

sedimentary rocks are the result of either precipitation of solids from solutions (like salt from water) or by organic process, like shells from marine organisms.

24
Q

FOLIATED

A

Metamorphic rocks that exhibit parallel alignments of minerals

25
Q

NON-FOLIATED

A

Metamorphic rocks composed of minerals that are not elongated or flat, do not exhibit parallel alignments

26
Q

SHALE

A

the most common sedimentary rock