CO6 GEO

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1

James Hutton

father of geology

bald

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Uniformitarianism

the present is the key to the past

This principle developed in the early 1800’s

led Earth scientist to realize the Earth was very old – at least

millions of years old

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actualism

more modern term of uniformitarianism

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numerical age

actual age given in years or other unit of time

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relative time

the sequence in which events took place

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Contacts

surfaces separating successive rock layers (beds)

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Formations

bodies of rock of considerable thickness with

recognizable characteristics allowing them to be

distinguished from adjacent rock layers

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relative age

order of events or objects, from oldest to youngest

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Original horizontality

beds of sediment deposited in water are initially formed as

horizontal or nearly horizontal layers

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Superposition

within an undisturbed sequence of sedimentary or volcanic rocks, layers get younger from bottom to top

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lateral continuity

original horizontal layer extends laterally until it tapers or

thins at its edges

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cross cutting relationships

a disrupted pattern is older than the cause of the disruption

• Intrusions and faults are younger than the rocks they cut through

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Baked contacts

contacts between igneous intrusions and surrounding rocks, where surrounding rocks have experienced contact metamorphism

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inclusions

fragments embessed in host rock are older than the host rock (»????)_

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uncomfortmities

surface (contact) that represents a gap in the geological record

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discomformities

the unconformity contact separates beds that are parallel

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Angular unconformities

the unconformity contact seperates a younger layer above from a lower layer that is tilted

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Nonconformity

an unconformity

in which an erosional surface on

plutonic or metamorphic rock has

been covered by younger

sedimentary or volcanic rock

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Correlation

The determination of

the time – equivalency of rock units

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Physical continuity

physically

tracing a continuous exposure of a

rock

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isotopic dating

puts absolute values

(for example, millions of years) on the

ages of rocks and geologic time periods

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Isotopes

varieties of the same element

that have different numbers of neutrons

in the nucleus

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Radioactive decay

the spontaneous

nuclear change of isotopes with

unstable nuclei.

• Alpha emission, Beta emission and

Electron capture

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Half-life

time it takes for a given

amount of radioactive isotope to be

reduced by half.

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Precambrian

represents 87 % of geologic time and is divided into

three Eons (Hadean, Archean, Proterozoic)

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Phanerozoic EON

most recent eon that includes all geologic time with

abundant fossil record

  • composed of

    • Paleozoic

    • Mesozoic

    • • Cenozoic

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James Ussher

“Earth created in 4004 B.C. based on the Bible”

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4.56 billion years

Today numerical dating gives age for Earth of _____

  • Earth and the rest of the solar system was very likely formed at this time

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Marine and transitional environments

are more favorable for fossil preservation than are continental environment, because the rate of sediment deposition tends to be higher

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Index fossils

aka guide fossils or indicator fossils

  • basis for defining boundaries in the geological time scale and the time correlation of strata

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Absolute Dating

It provides a method for measuring geologic time

directly in terms of a specific number of years

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Alpha particles

may be emitted from

the nucleus. ___________ consists of

two protons and two neutrons. After

emission, the mass number of isotope is

reduced by four and the atomic number is

decreased by two.

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beta particle

When _______ or electron is

given off from a nucleus, the mass

number remains unchanged because

electrons have practically no mass. The

atomic number increases by one because

the nucleus contains one more proton

than before

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Eon, Era, Period, Epoch, Age

geological time scale from longest to shortest

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Precambrian

  • Hadean

  • Archean

  • Proterozoic

_ 87% of earth’s history

  • named after hades

    • • The Earth undergone differentiation

      • The Moon formed (perhaps based on the Impact Theory)

      • The surface was an ocean of magma until 4.4 Ga based on zircon

      • Outgassing occurred forming the first ocean

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Archean Eon

“Beginning”

- Starts at around 3.85 Ga where there is a substantial

amount of crustal rocks.

The advent of the _____ marked the time when the

crust was locally cool and stable for rocks to survive

  • plate tectonics occured at this time

by the end of this eon, 80% of the earth’s continental land had formed

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Stromatolites

developed at around 3.2 Ga due to

cyanobacteria secreting a mucus-like substance to

which sediment settling from water sinks.

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Stanley Miller

an exobiologist,

achieved the laboratory

synthesis of amino acids.

• He simulated the early

atmosphere in a laboratory

flask and then sent sparks of

electricity into the mixture.

• The liquid yielded amino acids

and other complex

compounds.

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PROTEROZOIC EON

• Spans from 2.5 Ga to 542 Ma

• Encompasses almost half of the Earth’s history

• The surface environment changed from fast-moving

plates, small continents, and an oxygen-poor

atmosphere to an environment similar to today’s world

• The continents formed by at slower rates

• The interior of continents started to cool and strengthen

thus becoming relatively stable

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Rodinia

first supercontinent on Earth, formed during 1 Ga

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Grenville Orogeny

Rodinia’s formation triggered a mountain building

event known as the _____

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Pannotia

Rodinia broke away and formed a short-lived supercontinent called ______

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Proterozoic

At the beginning, life on earth was ______

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BANDED IRON

FORMATIONS

Alternating

layers of quartz

and iron rich

layers

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CRYOGENIAN GLACIATION

Near the end of the Proterozoic, 90% of entire Earth was

covered in ice in an event known as the _________ OR SNOWBALL EARTH

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The Great Ordovician Biodiversification Event

occurred 40 million years after the Cambrian Explosion

• New species, genus, family, and order different

taxonomic levels diversified.

• The first crinoids and first vertebrate animals (the

jawless fish) appeared during this time.

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Antler Orogeny

the west of the US collided with an island arc

thus causing the ________—

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SILURIAN PERIOD

Early land plants appeared during this time.

• The first jawed fish evolved known as the Acanthodians

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devonian period

• Age of the Fish

• First Amphibians

• First Insects

• Mass extinction near the end of this period

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CARBONIFEROUS PERIOD

First appearance of gymnosperms

• Proliferation of coal-forming swamps

• Diversification of amphibians

• Appearance of reptiles

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Permo-Triassic Extinction

The largest mass extinction in the Earth’s history.

  • happened in permian period

• 95% of marine species died

• One hypothesis is due to massive volcanism in now

Siberia where volcanic flood basalts formed known as

“Siberian Traps”

  • PANGEA WAS FORMED

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ORNITHISCIANS

• Bird-hipped dinosaurs

  • BIRDS DID NOT EVOLVE FROM THEM

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SAURISCHIAN

• Lizard-hipped

dinosaurs

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CAMBRIAN EXPLOSION

A remarkable diversification of life occurred during this

time.

• The reason for the abrupt diversification of life during

this time is unknown for certain.

• However, it is known that the evolution of hard parts

such as shells occurred this time as well the rise of new

phyla

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ORDOVICIAN MASS EXTINCTION

Due to a brief glaciation and associated sea-level

lowering, a mass extinction occurred at the end of the

Ordovician period.

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Triassic period

appearance of the first mammals

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Jurassic Period

  • during this period, ammonites began to be very abundant

  • aka the age of the ammonites

  • appearance of the first feathered birds

  • start of the great diversification of dinosaurs

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Cretaceous Period

peak of the dinosaur evolution

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KT boundary

boundary between crataceous and paleogene (pg)

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Mesozoic Mass extinction

dinosaurs vanished along with 90% of plankton species and up to 75% of plant species

The cause is likely due to the aftermath of a meteorite

impact as evidenced by high concentrations of Iridium

(normally found in meteorites)

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Chicxulub crater

A 16-km-deep meteorite crater is found in Mexico

known as _______

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CENOZOIC ERA

Subdivided into several epochs

Three periods

• Paleogene

• Neogene

• Quaternary

The appearance of Earth gradually

produced what we could see

today

  • Formation of the largest orogenic

    belt due to the closure of the

    Tethys Sea forming the AlpineHimalayan Chain.

  • The predominance of mammals wherein they would

    dominate.

    Dominance of angiosperms

    First appearance of:

    • Horses (Eocene Epoch)

    • Primates and Monkeys (Eocene Epoch)

    • Whales (Eocene Epoch

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PLEISTOCENE

ICE AGE

• 1/3 of the Earth’s

surface was covered in

ice

• Sculpted many

glaciated terranes

• Cause could have

been due cycles in the

Earth’s movements

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MILANKOVTICH

CYCLES

  • changes in the earth’s precession, orbital eccentricity, and axial tilt

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Precession

• Way the Earth’s axis

of rotation wobbles

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Orbital Eccentricity

The orbital path

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Weather

describes what the atmosphere is doing over

short timescales

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Climate

– the average weather pattern in a region over long

periods of time

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Anthropogenic Climate Change

climate change related to

human activities

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Thermosphere

also called the

ionosphere

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Albedo

percentage of radiation reflected from the surface

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Blackbody radiation

the intensity and wavelength of emitted

electromagnetic radiation depends on temperature

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Greenhouse gases

include water vapor, carbon dioxide, methane,

nitrous oxide, and other

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Milankovitch Theory

Changes in Earth’s orbital patterns

determine input and distribution of solar radiation over long

time scales

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41,00

the tilt of Earth’s axis varies on a ______ year

timescale

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Sunspots

are dark areas on the Sun’s surface that are hotter than

average

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30

Approximately __% of the Sun’s

radiation is reflected back into

space

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Climate feedback

conversion

of high albedo snow and ice to

lower albedo surfaces

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true

Snow and Ice have high

albedo (true/false)

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true

Darker surfaces have lower

albedos (true/false)

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Atmospheric lifetime

each

greenhouse gas survives in the

atmosphere for different amounts of

time

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Global Warming Potential

a relative

measure of each gases ability to trap

heat in the atmosphere

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Aerosols

small particles suspended in the

atmosphere.

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Volcanoes

releases particles and gases into the

atmosphere

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Plate tectonics

alters surface albedo and ocean

circulation over million-year timescales

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Paleoclimatology

the study of ancient climates

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Borehole thermometry

measuring

temperatures deep in the ground

to infer what temperatures must

have been in the past.

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Geoengineering

• Large-scale intentional efforts to modify Earth’s climate

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