Introduction Lec 1. Flashcards

1
Q

3 Principal Themes in Earth History

A
  1. Deep time –> geologic time scale
  2. Plate Tectonics
  3. Evolution of life
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2
Q

Leonardo da Vinci

A

First to recognize that mountains were not always there by seeing sea fossiles on top of mountains.

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3
Q

Robert Hooke

A

Hunch back that thought of Bio Strat and see that there was a chronology to fossils

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4
Q

Niels Stenson AKA Steno

A

Father of geology
Was called to cut open a shark and saw that the shark teeth matched “Giant” teeth found on the mountions
4 Steno Principles

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5
Q

Stenos 4 basic princibals

A
  1. Superpostion –> older rocks lie under unger rocks. Rocks can be tilited but there are ways of determinin the “way up” like animal burrows, mud cracks, pillow basults
  2. Original Horizontallity –> beds are deposited horizontally
  3. Original Lateral Continuity –> Rock layers extend laterally until physically constrained in some way
  4. Cross cutting relationships–> things that cross others are younger (like a sill or a dyke)
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6
Q

James Hutton

A

Uniformintarianism
saw that geologic process happend slowly by looking at his farm and seening nchent erroded rivers
Saw that the therory that the earth was formed by the big flood (the Big Deluge) was wrong

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7
Q

“Actualism”

A

Modifing how things are created from an evolutionary point of view.
Ex: how seed bearing grasses did not evolve tell the upper cretaceous and these seed bearing grasses are the reson for salt marshes

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8
Q

Sir Chales Lyell

A

Thought of “Deep Time” and that mountain bulding and erosion took long periods of time

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9
Q

William Smith

A

Father of Stratigraph!!!!

made the fisrt stratographic map =D

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10
Q

Henry Clifton Sorby

A

A scoop full of sediment
Father of sedimentology
first to view a thin section

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11
Q

Amadeus Grabau

A

Published papers way befor his time

First Geological survay of china and he was killed by japs!!!!!!!

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12
Q

When did sedimentology truly start?

A

Sedimentology truly started in 1950 b/c of Kuenen and Migliorini (ittalian guy)
Sedimentary features modeled in a lab
Modern land forms could be explaned with processes of old (uniforminatianism)

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13
Q

Graded Bedding

A

Usually with rivers/ turbidity currents coarse sand deposits first then fine sand than silt and clay. So the fines of the grains increases as you move up the unit.

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