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Lecture 1: Logistics and Science

Historical Geology

  • Age of Earth: ~4.54 billion years (± 0.05 billion years)

  • To understand Earth’s past, we use forensic analysis and observations to determine who, what, how, and why.

  • Uniformitarianism: the geological principle that the processes occurring in the present have operated in the same manner and at similar rates in the past.

  • We can determine a lot about the Earth using fossil records and geologic time.

Past Provides Clues for Our Future

  • Dinosaurs appeared at the end of Cretaceous

  • ~90% species disappeared at the Triassic/Permian boundary

  • Animals suddenly appeared

Maps

  • Topographic Maps: detailed, accurate graphic representations of features that appear on the Earth's surface, showing both natural and man-made elements, including elevation contours to represent the shape and height of the terrain .

    • Close lines indicate steep slopes while further apart lines are lines of equal elevation.

  • Geologic Maps: detailed representations of the distribution, nature, and age of rock formations and other geologic features on the Earth's surface.

  • Cross-sections: vertical profiles that show a side view of the arrangement and relationships of rock layers and geological features beneath the Earth's surface.

    • May show features such as layers of rock formations, intrusions, water flow, etc.

Scientific Method

What is Science?

  • Science uses observations, experiments, and calculations to explain how something works

  • Critical thinking needed to get verifiable results

Scientific Method

  • Recognize a problem and/or make an observation

  • Collect data

  • Form a hypothesis

  • Test hypothesis through experiments (field work, labs, etc.)

  • Validate or refute hypothesis

  • Revise hypothesis and retest again if needed

Scientific Theory

  • Theory: a hypothesis that has not yet been proven wrong; abundance of evidence. Explains how and/or why things happen; can be used to make predictions. Arises from tested hypotheses.

Scientific Law

  • Law: A concise statement of what will happen, but does not explain how or why they work.

Three Great Themes in Earth History

Deep Time

  • Deep time: immense amounts of time

Plate Tectonics

  • Plate tectonics: the large-scale deformation of rocks in Earth's outer layers, serving as a comprehensive theory that explains many geological phenomena.

Evolution of Life

  • Evolution: unifying theory for understanding history of life

  • Fossil records help us understand changes through time

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Lecture 1: Logistics and Science

Historical Geology

  • Age of Earth: ~4.54 billion years (± 0.05 billion years)

  • To understand Earth’s past, we use forensic analysis and observations to determine who, what, how, and why.

  • Uniformitarianism: the geological principle that the processes occurring in the present have operated in the same manner and at similar rates in the past.

  • We can determine a lot about the Earth using fossil records and geologic time.

Past Provides Clues for Our Future

  • Dinosaurs appeared at the end of Cretaceous

  • ~90% species disappeared at the Triassic/Permian boundary

  • Animals suddenly appeared

Maps

  • Topographic Maps: detailed, accurate graphic representations of features that appear on the Earth's surface, showing both natural and man-made elements, including elevation contours to represent the shape and height of the terrain .

    • Close lines indicate steep slopes while further apart lines are lines of equal elevation.

  • Geologic Maps: detailed representations of the distribution, nature, and age of rock formations and other geologic features on the Earth's surface.

  • Cross-sections: vertical profiles that show a side view of the arrangement and relationships of rock layers and geological features beneath the Earth's surface.

    • May show features such as layers of rock formations, intrusions, water flow, etc.

Scientific Method

What is Science?

  • Science uses observations, experiments, and calculations to explain how something works

  • Critical thinking needed to get verifiable results

Scientific Method

  • Recognize a problem and/or make an observation

  • Collect data

  • Form a hypothesis

  • Test hypothesis through experiments (field work, labs, etc.)

  • Validate or refute hypothesis

  • Revise hypothesis and retest again if needed

Scientific Theory

  • Theory: a hypothesis that has not yet been proven wrong; abundance of evidence. Explains how and/or why things happen; can be used to make predictions. Arises from tested hypotheses.

Scientific Law

  • Law: A concise statement of what will happen, but does not explain how or why they work.

Three Great Themes in Earth History

Deep Time

  • Deep time: immense amounts of time

Plate Tectonics

  • Plate tectonics: the large-scale deformation of rocks in Earth's outer layers, serving as a comprehensive theory that explains many geological phenomena.

Evolution of Life

  • Evolution: unifying theory for understanding history of life

  • Fossil records help us understand changes through time