Lecture 3 Flashcards

1
Q

Graphite and diamonds result of

A

different bonding

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2
Q

Mineral pairs most abundant in

A

basalt pyroxene and p

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3
Q

Fast cooling magma produces

A

aphanitic texture

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4
Q

Phenocrysts in a porphytic texture reflects

A

slow cooling

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5
Q

Basalts are the most common

A

EXTRUSIVE rocks on earth

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6
Q

Glassy texture are the product

A

lower nucleation and lower growth rates than apaphanitic texture

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7
Q

Pahoehoe

A

ropy lava

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8
Q

Pillow lava

A

Formed in aqueous environment

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9
Q

Main gases

A

H2o so2 co2

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10
Q

How do volcanoes explode?

A

Gasses= volitaile
Gas is trapped under pressure in magma chamber
conduit is plugged
when conduit released pressure explodes

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11
Q

Volcanic gas

A

Gas bubbles trapped in cooled volcanic rock.
Gas bubbles called vesicles.
The way the gas escapes determines what kind of eruption

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12
Q

low-viscosity basalt

A

Easier for gas to escape smaller eruption

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13
Q

high-viscosity rhyolite

A

Hard for gas to escape =big eruption

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14
Q

Fumaroles

A

vents or openings at the surface where volcanic gases and vapors are emitted.

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15
Q

Pyroclastic material

A

Pyro = fire and clastic = fragment

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16
Q

Bombs

A

> 64mm
Aerodynamic ribbon
solidifying globs of lava as it travels through the air

17
Q

Lapilli

A

Dark basaltic
called cinder
2-64mm

18
Q

Ash

A

<2mm
fine

19
Q

block

A

Exactly what it sounds like

20
Q

cinder cone

A

Smallest type of volcano
cone-shaped piles of ejected lapilli-sized
fragments
built up around vent
symetrical
deep crater

21
Q

Weathering/erosion

A

Active=smooth cone
Erosion=gullies
Eventually= hills of volcanic rock

22
Q

Size of volcano

A
  • volume of eruption vs. erosion
    Age/rate
23
Q

basalt

A

Fine-grained = aphanitic (super fine minerals)= rapid cooling

24
Q

How do we describe (and classify/name) a rock?

A

Mineralogy: type of minerals
texture: grain/crystal size
variability

25
Q

petrography

A

the study of rocks in thin sections by means of a petrologic microscope

26
Q

Glass

A

no mineral
very fast cooling

27
Q

Graph

A

slide 25

28
Q

Porphyritic texture

A

an igneous rock texture in which large crystals are set in a finer-grained or glassy groundmass.

29
Q

important elements

A

si, Al, Fe, Mg, Ca, Na, O

30
Q

Mineral

A

Minerals have a specialized
geologic definition. They are
naturally occurring, (mostly)
inorganic crystalline solids
formed by geologic processes
and with a definite chemical
composition.

31
Q

Chemical bonding and mineral formation

A

atomic packing and the nature of chemical bonding determine the mineral properties

32
Q

Crystal structure: polymorphs ( different crystal forms of the same compound)

A

ex.
Diamond and graphite are
polymorphs of carbon

33
Q

Silica tetrahedron

A
  • The SiO44− anionic unit is also known as the silica tetrahedron, a fundamental
    building block of silicate minerals.
  • The silica tetrahedra can be depicted in several ways: as an atomic diagram, a
    ball model, a ball and stick model, or as a geometric sketch.
34
Q

Pyroxene, Diopside:

A

CaMgSi2O6

35
Q

Olivine

A

(Mg,Fe)2SiO4
Forsterite: Mg2SiO4
Fayalite: Fe2SiO4

36
Q

Plagioclase feldspar

A

(Ca,Na)Al1-2Si2-3O

37
Q

Albite

A

NaAlSi3O8

38
Q

Anorthite

A

CaAl2Si2O8

39
Q

Quartz

A

SiO2