Chapter 1: Earth as a System Flashcards
Principles of Actualism
fundamental physical & chemical principles observed operating today have operated throughout Earth’s history
Catastrophism
global floods caused by supernatural forces formed most of the rocks visible at Earth’s surface.
- Attribute all layers of rocks to series of catastrophes
Principles of Uniformitarianism
present is key to the past
- Somewhat rigid view of Earth’s eternal processes
§ Ex: no events played important geological role - denied by impact of asteroid
§ Ex: all geological changes are gradual - denied by numerous agents which operated with suddenness
§ Ex: all kinds of rocks have never basically changed - denied by new kinds of rocks & organism appear, mammals existed in only 5 percent of planet’s history.
Mineral
Naturally occurring Inorganic Solid Element/ Compound Particular chemical composition Characteristic mineral structure/ Crystal lattice
Rock
consist of interlocking or bonded grains of matter - typically composed of single minerals
Igneous
cooling of molten materials
Sedimentary
bonding of loose sediments by compression after burial or precipitation of mineral cement - result of lithification of sediment
Metamorphic
alteration of rocks within Earth under conditions of high temp & pressure
Steno’s Law: Principle of Superposition
in an undisturbed sequence of data - oldest at bottom & successively higher strata are progressively younger
Steno’s Law: Principle of Original Horizontality
all strata are horizontal when they form
Steno’s Law: Principle of Lateral Continuity
strata originally are unbroken flat expanses, original continuity can be broken by erosions (ex: when river cuts downward)
Principle of Intrusive Relationship
intrusive igneous rock is always younger than the rock that it invades
Principle of Inclusion
when fragments of one body of rock are found within a second body, the 2nd is always younger than the 1st.
Unconformity
irregular surface between two bodies of rock
Angular Unconformity
a group of rocks has been tilted & eroded & younger rocks are deposited on top
Disconformity
the irregular surface between the upper & lower rock bodies reveals a past episode of erosion
Nonconformity
a bedded rocks rest on an eroded surface of crystalline (igneous/ metamorphic) rocks
Fossil
tangible remains/signs of ancient organism
Geological Time Scale
Divides Earth’s history into formal units (see side pic)
Divides by the levels in which geologist discover abundant fossils
Eons, Eras, Periods, Epochs
Geological systems
□ Unique group of fossils
□ Nature of rock
Core
Solid, spherical inner portion
Liquid outer portion - consist mostly of iron
Mantle
§ Thick envelop around core
§ Complex body of less dense rocky materials
§ Made up most of Earth’s volume
Crust
still less dense (than mantle & core) rock material
Moho - Mohoroviěié discontinuity
passage between crust to mantle where waves increase in velocity abruptly
Lithosphere
crust & upper mantle
Asthenosphere
“low-velocity zone”, composed of partially molten rock, slush like, solid particles with liquid occupying in between, 10% thickness of mantle
Basics of Plate Tectonic
the movement of lithospheric plates; driven by convection (process by which material that is heated deep within the asthenosphere rises to displace cooler, less dense material near surface)
Type of boundary: Spreading Zones
plates move apart, mafic material of relatively low density rise from ultramafic asthenosphere and become new lithosphere, lithosphere slide laterally away
□ Ex: Mid-ocean ridge (Mid-Atlantic)
Type of boundary: Subduction Zones
plates move back down the asthenosphere along deep-sea trenches
Type of boundary: Transform Faults
plates slide along each other; faults offset mid-ocean ridges throughout their length
Water Cycle
see OneNote
Darwin’s Theory of Evolution
particular kinds of animals & plants gave rise to other kinds
- cyclical but progressional, constantly giving rise to new kinds of organisms
Directional changes: Physical
cooling of planet’s interior - weakened furnace, plate tectonic weakened, less subduction & spreading zones
Directional changes: Chemical
shifts of oxygen concentration
Ecosystem
an environment together with the group of organisms that lives within it.
- Environmental change influenced ecosystems. Study of ancient ecosystems let geologists know how to confront future environmental changes.