Lecture 4 - Geology Flashcards

1
Q

rock types

igneous

A

cooling of magma, contains datable minerals

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2
Q

rock types

sedimentary

A

accumulation of particles

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3
Q

rock types

clastic

sedimentary

A

particles are weathered bits of other fossils
- sandstone, conglomerate, breccia

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4
Q

rock types

organic

sedminetary

A

particles are animal/plant debris (CaCO3 etc), especially in shallow water

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5
Q

rock types

creation of sedimentary rock

A

filling of low lying areas (basins); action and speed of water flow is key - determines size/density of particles deposited

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6
Q

rock types

chemical

sedimentary

A

particles are dissolved minerals that precipitate directly from suspension

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7
Q

fossils

fossil definition

A

mineralized remains of an organism, or impression of the organism
in terrestrial settings, usually occurs in clastic sedimentary rock

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8
Q

fossils

process of fossilization

A

death, neglect, burial, fossilization

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9
Q

stratigraphy

strate

A

layers of rocks

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10
Q

stratigraphy

principle of original horizontality

A

strate are layed down horizontally originally, any tilt happens after they are laid down

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11
Q

stratigraphy

principle of lateral continuity

A

chemically identical beds are part of the same layer of rock bed, even if later moved on

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12
Q

stratigraphy

law of superposition

A

older layers at the bottom, younger on top

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13
Q

stratigraphy

principle of cross-cutting

A

cross-cutting layers can only cut existing layers, so it is younger than those it cut

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14
Q

stratigraphy

principle of faunal succession

A

use biological organisms present in fossil bed to determine age of strate

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15
Q

stratigraphy

index fossils

A

organisms that are more specific to a certain time period/relatively constrained times - more indicative of the age of strata

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16
Q

absolute dating methods

14C dating

A

estimate age based on proportion of remaining 14C
- half-life = 5730 years
- becomes negligible after 50k years

17
Q

absolute dating methods

K-Ar Dating

A

decay of 40K to 40 Ar
- Ar gas escapes liquid magma, but accumulates as magma and hardens (Ar “zeroed” out at eruption)
- half-life = 1.3 billion years

18
Q

absolute dating methods

tephra

A

bed formed by volcanic ashfall
contains glass & minerals that can be directly dated

19
Q

absolute dating methods

magnetostratigraphy

A

earth’s core is magnetic, measure of mineral alignment to understand magnetic field = placement of time