Introduction Course overview History of Oceanography Intro to Earth.

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Introduc tion Course overview History of Oceanography Intro to Earth

Transcript of Introduction Course overview History of Oceanography Intro to Earth.

Page 1: Introduction Course overview History of Oceanography Intro to Earth.

Introduction

Course overview

History of Oceanography

Intro to Earth

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Course web page

chem.winthrop.edu Click on Courses on left column Find GEOL 220 link

Syllabus, topic outlines, schedule, etc.

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Interdisciplinary

Biology Chemistry Physics Geology Geography Political Science Mathematics Computer Science

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History of Oceanography

Early Middle Ages Age of Discovery Discovery with Science Modern Oceanography

Different motivations at different times

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The Oceans

Atlantic Pacific Indian Arctic Southern Ocean

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Early history

Reasons: trade, fishing, defense

Self centered view of Earth Examples

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Early history (2)

Difficult to navigate without shorelines Phoenicians (approx. 1000 BC)

Polynesians (300-600 AD most important)

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Early history (3)

Greeks (approx. 500 BC)– Erasthosthenes (working in Egypt) –

circumference of earth– Pliny the Elder – phases of moon and tides– Ptolemy (approx. 150 AD) – vast ocean, used lat

and long

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Middle Ages

Very little exploration except

Vikings (approx. 1000 AD)

Arabs

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Age of Discovery (1)

Travel for economic, political and religious reasons

Portugal: – Prince Henry– Dias (1497)– Vasco Da Gama (1498)

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Age of Discovery (2)

Spain Columbus (1492) Vespucci (~1500) Balboa (1513) Magellan (1522)

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Discovery with Science

Discovery with some science James Cook (1768-1780) Ben Franklin (1769) Matthew F. Maury (early 1800s)

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Purely scientific Challenger Expedition (1872-1876) Extremely significant

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More for science

Voyages of Nansen aboard Fram (end of 1800s)

Meteor expedition (1925-27)

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Modern Oceanography (since 20th century)

International Interdisciplinary Scientific Complex instruments “Modern” technology

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Modern Oceanography

US funding Oceanographic institutes Drill ships, satellites, for example International cooperation

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Origin of solar system: nebular hypothesis

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Layered Earth

Density stratification

Core MantleCrustOceans and Atmosphere

Lithosphere Asthenosphere

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Geologic time

Details not important here Vast length of time very important Compare to human time