Rock Determination HydroGeo Flashcards

1
Q

The three types of rocks

A

igneous, metamorphic, sedimentary

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2
Q

What are the two types of igneous rocks and how were they formed?

A

intrusive - formed in earth, solidified slowly, small minerals
extrusive - cooled quickly outside the earth, coarser minerals

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3
Q

What is the basic silica structure?

A

SiO4 - this has a charge of -8 and is often compensated by Fe or Mg. This is known as the olivine group

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4
Q

What is the pyroxene group?

A

one line of SiO4 minerals

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5
Q

What is the amphibole group

A

a layer of double structures

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6
Q

What are phyllosilicates?

A

platy minerals

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7
Q

What is the tectosilicate group?

A

a 3D structure

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8
Q

What are felsic igneous rocks?

A

extrusive rocks formed from explosive volcanoes - higher SiO2

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9
Q

What are mafic igneous rocks?

A

Extrusive rocks formed from fluid volcanoes - lower SiO2

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10
Q

When does weathering occur more quickly with rocks?

A

When there are more metals - these are easier to weather than chemical bonds - van der Waals forces are easier to break than chemical bonding

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11
Q

Granite

A

intrusive igneous rock. Lightly coloured with a mix of light and dark silicates. Mainly light minerals. The darker minerals weather first. Same chemical composition as rhyollite. Weathers slower than rhyollite, unless fractured

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12
Q

Diorite

A

Intrusive Igneous Rock. 50/50 distribution of light and dark silicates. Doesn’t weather fast. Same chemical composition as Andesite

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13
Q

Gabbro

A

Intrusive igneous rock. Predominantly large dark minerals. Same chemical comp. as basalt , but weathers slower (larger minerals) unless fractured.

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14
Q

Rhyolite

A

light extrusive igneous rock. Small minerals, high viscosity when forming. Rare, so usually solidifies inside the earth. Weathers faster than granite –> smaller minerals

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15
Q

Andesite

A

50/50 extrusive igneous rock. Has more dark minerals than rhyolite. Twins with diorite

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16
Q

Basalt

A

dark extrusive igneous rock. Lots of metal ions. Rock forms in polygones during cooling and solidification process. The scrambled egg on top has higher porosity, volcanic gas causes bubbles.

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17
Q

Tuff

A

volcanic ash and lava bombs fall back on the earth. When it cools in the air, aquifer, when it cools on the surface, aquitard.

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18
Q

Two types of diagenesis

A

reduction of volume (compression/compaction at large depth), mineralogical change (chemical processes between core and water minerals)

19
Q

eg. consolidated coarse clastic sediment

A

conglomerate

20
Q

eg. consolidated moderately coarse clastic sediment

A

sandstone

21
Q

eg. consolidated fine clastic sediment

A

siltstone, shale

22
Q

arenite

A

consolidated rocks constructed from sand size particles.

23
Q

lutite

A

consolidated rocks with smaller than sand size grains

24
Q

rudite

A

consolidated rocks with larger than sand size grains

25
Q

organic vs. clastic limestone

A

organic - chalk skeletons of algae, sea shells and organisms, clastic is from transported skeleton gragments or from calcite crystals.

26
Q

slate

A

fine grained rock, developed from clayk strong cleavage preference in one direction.

27
Q

Phyllite

A

slightly coarser rock than slate with silvery or greenish lustre, minerals not visable, developed from low graded metamorphosed clay

28
Q

Schist

A

coarse grained rock with parallel structures and clearly visible micas.

29
Q

Gneiss

A

coarse grained with clearly visible parallel structures of micas and fedspars, characterized by coarse layering. High grade metamorphose. no porosity or conductivity

30
Q

Granite to sand (types of sand)

A

monocyclic sand - darkest minerals weather fter - weaker van der Waals forces.
polycyclic sand - multiple cycles of weathering - even fewer darker minerals.

31
Q

sand to sandstone

A

poorly consolidated - still has porosity- to highly consolidated (no pores). high pressure and temp required. sandstone weathers faster than rain.
you can still see sand in sandstone

32
Q

quartzite to magma

A

make it hotter

33
Q

silt to siltstone

A

silt –> consolidated siltstone (sedimentary) –>highly consolidated siltstone (metamorphic)

34
Q

gravel to conglomerate to quartzite

A

gravel –> burial and lithification –> conglomerate –> breccia –> quartzite
Metamorphic -> high temp, pressure, long time.

35
Q

clay to shale

A

burial and lithification - pushed in same direction

36
Q

shale to phyllite to slate

A

metamorphic formation, dull colours

37
Q

shale to schist

A

metamorphic –> colourful.

38
Q

granite to gneiss

A

metamorphic

39
Q

carbonate sequencing

A

calcium carbonate –> cretaceous chalk –> carboniferous limestone

40
Q

hardness

A

on a scale of 10 - silica dominated is roughly 6-7, chalk is 3

41
Q

limestone –> marble

A

no porosity or hydraulic conductivity anymore, still on chalkboard :)
metamorphic transformation

42
Q

Flintstone

A

silica skeleton creatures, found in chalk

43
Q

gypsum

A

calcium sulphate