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Geology Study Guide

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Geology Study Guide
GEOLOGY 101 Exam 1 Study Guide Geology | * The science that examines Earth, its form and composition, and the changes that it has undergone and is undergoing * The processes are slow, but none the less dynamic * Physical geology: examines Earth materials and seeks to understand the many processes that operate on our planet * Historical geology: seeks an understanding of the origin of Earth and its development through time | Scientific Method | * It is a rigorous process whereby new ideas about how some part of the natural world works are put to the test * The result of testing must be reproducible * It is believed that the universe is orderly and that by observing it objectively, we can learn how it works * How does testing take place? * Starts with a question * Collect evidence/data that answers the question | Hypothesis | * A tentative conclusion/explanation about natural processes being questioned * It can be revised/changed as needed * Scientists are actually trying to prove the conclusion wrong | Scientific Theory | * A conclusion/explanation that is supported by experimental or factual evidence but has not been conclusively proved * Theories explain the data in a concise manner * Example: E = mc2 theory of relativity | Natural Law | * Never ever false | Alfred Wegener | * “Father of Plate Tectonics,” German meteorologist * Introduced his hypothesis in “Origins of Continents and Oceans” in 1915 * Suggested that a super continent called Pangaea (all lands) existed during most of the Paleozoic * 200 Ma (Mz) Pangaea began breaking up into smaller pieces (continents) and moved to their present location | Evidence that supports continental drift | * Fit of continents looked like pieces of a puzzle * Fossils * Mesosaurus: snaggle toothed reptile; found exclusively in South America and Africa; lived in fresh water * Glossopteris: seed fern associated with polar climates; found in

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    In 1912, Alfred Wegener published his theory that a single super continent named Pangaea once existed about 300 million years ago. He proposed that Pangaea then later split into two continents of Laurasia in the north and Gondwanaland in the south and that today’s continents were the result of further splitting of these two land masses. Where the plates split are known as plate boundaries. Wegener’s theory of continental drift was supported by both geological and biological evidence that these areas were once joined. The geological evidence included the rock sequences in Northern Scotland closely agreeing with those found in East Canada, indicating that they were laid down under the same conditions in one location as well as the obvious jig saw fitting appearance of today’s continents, in particular, the bulge of south America fitting into the indent below west Africa. The biological evidence comprised of fossil findings linking different continents. Fossil brachiopods found in Indian limestones were comparable with similar fossils in Australia and the fossil remains of Mesosaurus’ were found in both South America and southern Africa. It is unlikely that the same reptile could have developed in both areas or that it could have migrated across the Atlantic. Despite the evidence, Wegener’s theory was unable to explain how continental movement had occurred. However from the 1940’s additional evidence accumulated after the discovery of the mid-Atlantic ridge and huge oceanic trenches. Examination of the ocean crust either side of the mid-Atlantic ridge suggested that sea-floor spreading was occurring. Magnetic surveys of the ocean floor in the 1950’s, showed regular patterns of paleomagnetic striping surrounding the ridges. It was discovered that when lava erupts on the ocean floor, magnetic domains within iron rich minerals in the lava are aligned with the…

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