Lecture 4 - Geology Flashcards
rock types
igneous
cooling of magma, contains datable minerals
rock types
sedimentary
accumulation of particles
rock types
clastic
sedimentary
particles are weathered bits of other fossils
- sandstone, conglomerate, breccia
rock types
organic
sedminetary
particles are animal/plant debris (CaCO3 etc), especially in shallow water
rock types
creation of sedimentary rock
filling of low lying areas (basins); action and speed of water flow is key - determines size/density of particles deposited
rock types
chemical
sedimentary
particles are dissolved minerals that precipitate directly from suspension
fossils
fossil definition
mineralized remains of an organism, or impression of the organism
in terrestrial settings, usually occurs in clastic sedimentary rock
fossils
process of fossilization
death, neglect, burial, fossilization
stratigraphy
strate
layers of rocks
stratigraphy
principle of original horizontality
strate are layed down horizontally originally, any tilt happens after they are laid down
stratigraphy
principle of lateral continuity
chemically identical beds are part of the same layer of rock bed, even if later moved on
stratigraphy
law of superposition
older layers at the bottom, younger on top
stratigraphy
principle of cross-cutting
cross-cutting layers can only cut existing layers, so it is younger than those it cut
stratigraphy
principle of faunal succession
use biological organisms present in fossil bed to determine age of strate
stratigraphy
index fossils
organisms that are more specific to a certain time period/relatively constrained times - more indicative of the age of strata
absolute dating methods
14C dating
estimate age based on proportion of remaining 14C
- half-life = 5730 years
- becomes negligible after 50k years
absolute dating methods
K-Ar Dating
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
absolute dating methods
tephra
bed formed by volcanic ashfall
contains glass & minerals that can be directly dated
absolute dating methods
magnetostratigraphy
earth’s core is magnetic, measure of mineral alignment to understand magnetic field = placement of time