390 likes | 898 Views
Introduction to Earth Science. Or, How The Earth Works. Branches of Earth Science. Geology Solid Earth Much Larger than Other Parts Many More Kinds of Materials Preserves a History Meteorology – Climatology Oceanography Astronomy Planetary Geology. The Earth Systems.
E N D
Introduction to Earth Science Or, How The Earth Works
Branches of Earth Science • Geology • Solid Earth Much Larger than Other Parts • Many More Kinds of Materials • Preserves a History • Meteorology – Climatology • Oceanography • Astronomy • Planetary Geology
The Earth Systems • External Effects (Astronomical) • Atmospheric Circulation • Oceanic Circulation • Hydrologic Cycle • Rock Cycle • Plate Tectonics
Earth and the Universe(external effects) • Earths’ Rotation (Day-Night) • Lunar Effects (Tides) • Annual Variation (Seasons) • Precession and Orbit Variations (Ice Ages?) • Galactic Rotation (250 m.y. period) • Unpredictable Events • Nearby Supernovae • Meteor Impacts • Long-Term Evolution of Sun
Atmospheric Circulation • Unequal Solar Heating • Equator to Pole • Day - Night • Different Surfaces • Buoyancy • Heating and Cooling • Coriolis Effect • High and Low Air Pressures • Fronts and Air Masses
Oceanic Circulation • Surface Currents - Driven by Winds • Thermohaline - Deep Circulation • Evaporation makes water more saline and denser • Freezing makes water more saline and denser • Cold water is denser than warm water
Hydrologic Cycle • Evaporation from Oceans • Precipitation on Land • Infiltration into Ground (Ground Water) • Runoff (Erosion)
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 • New Rocks Exposed by Erosion • Rocks Broken Down Mechanically and Chemically (Weathering) • Components Transported by Erosion • Components Cemented into Sedimentary Rocks • Burial and Heating creates Metamorphic Rocks • Melting Creates Igneous Rocks
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
Configuration of Continents • Oceanic Circulation • Weather and Climate Patterns • Deserts • Mountains and Rain Shadows • Pathways for Migration • Ecological Niches
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.
1 Second = 1 Year • 35 minutes to birth of Christ • 1 hour+ to pyramids • 3 hours to retreat of glaciers from Wisconsin • 12 days = 1 million years • 2 years to extinction of dinosaurs • 14 years to age of Niagara Escarpment • 31 years = 1 billion years
Some Unique Aspects of Geology (Continued) Reliance on Inference and Deduction Intrinsically "Unsolvable" Problems • Ancient Landscapes • Mass Extinctions • Ancient Ocean Basins
Scientific Principles in Geology • Parsimony (Keep It Simple) • Superposition • Uniformitarianism Using these, plus observation, we establish facts about Earth Processes
Parsimony • The simplest explanation that fits all the data is preferred • Doesn’t guarantee that things must be simple! • Theories with lots of ad hoc or unsupported ideas are probably wrong.
Uniformitarianism Continuity of Cause and Effect • Apply Cause and Effect to Future - Prediction • Apply Cause and Effect to Present - Technology • Apply Cause and Effect to Past - Uniformitarianism