Geology

66 important questions on Geology

New hypotheses not accepted without consideration by peers, rigorous testing

Peer Review

-Challenging concept
-Ultimate challenge - determine the age of Earth
-Many ideas based in religion and philosophy
-Scientific evidence --> the rock record

Deep Time

Radioactive decay rates of about ___elements found on Earth, Moon, and Asteroids

15 elements
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-Rocks can be ordered
-Rocks can be interpreted
-Rocks can be dated

The Rock Record

At __ Ma, visible life appears in the rock record

550

-Life becomes increasingly diverse (and bigger), moves onto land
-Lifestyles of modern organisms begin to appear

550-65 Ma

-Multi-cellular organisms with shells and claws
-Predator-prey relationships recorded in fossils

550 Ma

-Preserves fossils of small organisms
-Primary producers - oxygen becomes available in seawater

Early Earth - The next two billion years

-Hold no evidence of any life
-Deformed rocks of the Archean Eon, when Earth was lifeless and devoid of free oxygen

Early Earth - the first two billion years

After 65 Ma, _____ take over after global catastrophe

Mammals

Rocks in ND hold an excellent record of ____ _____ and ______ ______ between 55 and 25 Ma ago

Climate change and mammal evolution

The rock records is where information for ____ _____, ___ ____, and ___ comes from

past conditions, life forms, and events comes from

The most abundant rocks and minerals consist of the most abundant _____

elements

A mineral based on Si + O is a

Silicate

Quartz is composed of the two most common elements

Silicon and Oxygen

Feldspars Si and O with the addition of K, Al, Na, Ca

Very common - 60% of the crust
Almost as durable as quartz

-Common in almost all rock types
-Very hard and very durable

Quartz

Quartz, potassium feldspar, muscovite
-MOST stable at Earth surface, LIGHT in color, MORE silicon and aluminum

Felsic silicates

Biotite, olivine, pryoxene, amphibole
-LESS stable at Earth surface, DARK in color, LESS silicon and aluminum

Mafic silicates

Product of cooling/freezing of liquid rock both above and below ground

Igneous Rock

Fragments of rock - sediment - being compressed and cemented (or minerals being precipitated)

Sedimentary Rock

Form when rocks are heated and squeezed so that structure/composition change

Metamorphic Rock

______ igneous cool slowly and minerals have time to grow large, visible mineral crystals

Intrusive Igneous

______ igneous rocks cool quickly and minerals have NO TIME to grow. (mostly) invisible minerals crystals

Extrusive Igneous Rocks

Silica ____ than ~60% creates fluid flows
-Flows can be so calm that you can walk up to some

less

Silica ____ than ~60% creates explosive eruptions
-Gases are trapped up in high Si magma, escapes at eruption

greater

____ sedimentary rocks are composed of fragments of other rocks
-Subdivided by grain size

Detrital Sedimentary Rock

Fragments >2 mm
-The pebbles are clearly visible to the eye

Conglomerate

Rocks comprised of CaCo3 (limestone)

Carbonates

1. Precipitate directly from seawater
2. Accumulations of animal shells

Carbonate Sedimentary Rock

What is an example of a carbonate rock?

Coral Reefs

Precipitate from evaporating seawater or lake water

Evaporites

What is an example of an evaporite mineral?

Table Salt

Evaporation of saturated water (3)

1. Halide
2. Sulfate
3. Crystalline

____ and _____ cause new minerals to grow without melting

Heat and Pressure

Wegner's observations and other ideas:

-Shapes of continents
-Discontinuous mountain belts
-Fossils of terrestrial organisms on separate continents

Adding to Wegner's observations made during WWII

-Magnetic properties of the seafloor

The magnetic field of Earth flips usually ___  or ___ switches/million years. Well-studied phenomenon

4 or 5

Mantle plume rises, molten material crystallizes to form ____

crust

New (young) rocks forming at _____, old rocks drifting away from it

MOR

Plates are crashing into each other over the sinking arm of a mantle convection cell

Convergent

- 5-10 km of mafic igneous rock, sediments on top
- Greater density (3.0 g/cc)
- Hot near MORs, colder and denser away from them

Oceanic Crust

- 30-50 km of felsic rock
- Lower density (2.7 g/cc)
- More buoyant and difficult to recycle at plate boundary

Continental Crust

1. The older, colder oceanic crust sinks - S zone
2. Forms a deep trench on the ocean floor
3. Subduction cause melting
4. A chain of volcanic island results

Ocean-Ocean Collision

1. Neither crustal plate sinks
2. Massive mountain ranges develop

Continent-Continent Collision

1. Crust of Earth broken into plates
2. Plates riding on convection cells in the mantle
3. New oceanic crust created at a rising arm/MOR
4. Oceanic crust destroyed at subduction zone
5. Plate growth/destruction happens at margins

The Basic Ideas:

-Sedimentary rocks are deposited on top of one another
-Form in environments similar to those where sediments (detrital and carbonates) are deposited today

Nicolaus Steno's Observations

Layer at top is youngest, layer at bottom is the oldest

Principle of Superposition

Sediments are deposited horizontally, then compressed to form sedimentary rocks

Principle of original horizontality

Layers of sediments initially extend laterally in all directions

Principle of lateral continuity

-Some rock layers do not conform with neighboring layers
-Rocks can have inclusions of other, older rocks
-Fossils preserved in rocks record life when the rocks formed

James Hutton's Observations (19th century)

Fragments of rock present in a rock are older than that rock

Principle of inclusions

Oldest fossils preserved in oldest rocks, younger fossils in younger rocks

Fossil Succession

Layers of material that form at a known rate and can be used to determine an absolute age

Countable Layers

Example 1 of countable layers:
pairs of growth bands form every year 
-Oldest about 5,000 years

Tree Rings

Example 2 of countable layers:
Counting layers in sediment cores indicates that these have existed for 20,000 years

Layers in mud in frozen lakes

Example 3 of countable layers:
Pairs of light and dark bands represent one year
-Counting layers in cores indicate that it is at least 850,000 years old

Layers of ice exposed in glaciers

Example 4 of countable layers:
Growth layers of this age up to 2 million years old

Layers in coral

Stable or unstable versions of elements

Isotopes

Carbon atoms with ___ or ___ neutrons are stable, they will last forever

6 or 7

The old atom was a  _____

Parent

Radioactive decay of parent to daughter isotopes rate is _______ over long time intervals

Consistent

Igneous rock/crystal becomes "____" when it solidifies

"closed"

Eons - Three that span all of Earth history

Phanerozoic (visible life)
Proterozoic (earlier life)
Archean (beginning)

Ends with major extinction event:
-All dinosaurs except birds
-All large marine reptiles
-All flying reptiles
-Several mammal groups

Period of the Mesozoic

Extinction: 90% of all marine species, 70% of terrestrial; only extinction event to ever hit insects; largest of all time (so far)

Period of the Paleozoic

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