How The Earth Works. The Solid Earth Earth Science Geology – Solid Earth Much Larger than Other Parts – Many More Kinds of Materials – Preserves a.

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Presentation transcript:

How The Earth Works

The Solid Earth

Earth Science Geology – Solid Earth Much Larger than Other Parts – Many More Kinds of Materials – Preserves a History Meteorology – Climatology Oceanography Astronomy – Planetary Geology

Earth Systems External Effects (Astronomical) Atmospheric Circulation Oceanic Circulation Hydrologic Cycle Rock Cycle Plate Tectonics

Earth Systems

Convection

Earth and the Universe Rotation (Day-Night) Lunar (Tides) Annual (Seasons) Precession and Orbit Variations (Ice Ages?) Galactic? (250 m.y. period) Unpredictable Events – Nearby Supernovae – Meteor Impacts Long-Term Evolution of Sun

Atmospheric Circulation

1905 Weather Map

Rotation Effects

Not a Manifestation of the Coriolis Effect! Too small scale for the Coriolis Effect to be significant

Early Map of Gulf Stream

Surface Currents

Thermohaline Circulation

Hydrologic Cycle

Water Principal Agent in Modifying Earth’s Surface Medium for Storing and Distributing Global Heat The Universal Solvent – Essential for Life – Destructive to Rocks Lowers Melting Point of Rocks Reduces Strength of Rocks Under Pressure

The Rock Cycle

Plate Tectonics Outer Crust of Earth Moves a Few cm/yr Driven by Convection in Earth’s Interior Accounts For: – Earthquakes – Volcanoes – Mountain-Building (Orogeny) Configuration of Continents

Plate Tectonics

Some Unique Aspects of Geology Importance of Relationships Sequential Spatial Importance of Time Distinctive Problems of Evidence Slow Rates Rare Events Destruction of Evidence Inaccessibility

Some Geologic Rates Cutting of Grand Canyon 2 km/3 m.y. = 1 cm/15 yr Uplift of Alps 5 km/10 m.y. = 1 cm/20 yr. Opening of Atlantic 5000 km/180 m.y. = 2.8 cm/yr. Uplift of White Mtns. (N.H.) Granites 8 km/150 m.y. = 1 cm/190 yr.

Some Geologic Rates Movement of San Andreas Fault 5 cm/yr = 7 m/140 yr. Growth of Mt. St. Helens 3 km/30,000 yr = 10 cm/yr. Deposition of Niagara Dolomite 100 m/ 1 m.y.? = 1 cm/100 yr.

Some Unique Aspects of Geology (Continued) Reliance on Inference and Deduction Intrinsically "Unsolvable" Problems: Mostly where Physical Evidence is Gone Ancient Landscapes Mass Extinctions Ancient Ocean Basins

Scientific Principles in Geology Parsimony (K.I.S.S.): No ad hoc explanations Superposition: Young processes overprint older ones Uniformitarianism: Continuity of Cause and Effect Using these, plus observation, we establish facts about Earth Processes

Superposition: Mindoro Cut, Wisconsin

Geologic Map