(NOT FINISHED 4.3) Unit 4: Earth Systems and Resources

(4.1) Plate Tectonics

PLATES + BOUNDARIES

  • Earth’s layers:

    • Lithosphere (crust)

    • Asthenosphere (upper mantle)

      • Oceans and land sit on top of layer

    • Mesosphere (lower mantle)

  • Convergent plate boundary: plates that push towards each other

    • Causes volcanoes, rising magma, and earthquakes, trenches, island arcs

  • Divergent plate boundary: plates that push away from each other

    • Has ridges/volcanoes

    • Causes seafloor spreading, hotspots

    • Less frequent earthquakes

  • Transform plate boundary (aka Strike-Slip): plates that push past each other in opposite directions

    • No ridges/volcanoes

    • Shallow/frequent earthquakes

    • Causes fault lines

  • Continental plates: plates that carry continents, earth, and rock

    • Less dense → float

  • Plates might have several boundaries with other plates → diverse geological features

    • Can have breaks in surfaces → volcanic island change

      • EX: Japan, Indonesia, Hawaii

GEOLOGICAL FEATURES 

  • Convection: movement of Earth’s tectonic plates that are driven by currents in the mantle layer

  • Earthquakes: movement in the Earth caused on fault lines/plate boundaries

    • Occur at transform boundaries

    • Fault lines lock up/press to each other → builds up stress → energy releases

  • Tsunamis: long sea wave that gets bigger as it reaches the coastline

    • Earthquakes, underwater landslides → tsunamis

    • Destroys habitats, drowns species, uproots trees, contaminates freshwater (w/ saltwater + debris) 

  • Subduction Zone: one plate gets pressed under another plate that rises above it

    • Occur at convergent boundaries

(4.2) Soil Formation + Erosion

SOIL

  • Parent material is weathered → transported → deposited → soil

    • Factors:

      • Type of parent material (soil contains the chemistry of the rock)

      • Climate (average temperature, moisture change of weathering, the nutrients in the moisture, and wind)

      • Topography (slope of land)

      • Biological factors (plants, animals, microorganisms)

      • Time (how long soil forms)

  • Parent material: original rocks that are broken down to form the base of soil

    • Done by Weathering: breakdown of rock

  • Soil profile (or Soil Horizons): layers of soil built up over time

    • O-horizon: organic matter

      • Contains organisms, leaf litter,

    • A-horizon: surface soil

      • Contains humus, organic material, some rock

    • B-horizon: subsoil

      • Surface soil but with more rock

    • C-horizon: substrata

      • Parent material

    • (R-horizon) = bedrock

EROSION

  • Soil erosion: topsoil is stripped away by wind, water, gravity

    • Human factors: 

      • Deforestation (lack of roots that hold down the soil → replaced by plants that worsen erosion like wheat or soybean)

      • Overgrazing (cattle overeating → exposes topsoil)

      • Pesticides/fertilizers (changes chemistry of soil + kills microorganisms in soil)

      • Tilling (breaking soil prevents topsoil from getting organic material/roots)

    • Sheet erosion: surface layer is removed by water

      • Solution: maintain plant coverage

    • Rill erosion: small channels of water flow soil away

      • Solution: strip cropping/contouring tilling (low tilling)

    • Gully erosion: wider cuts in soil from expanded rill erosion

      • Solution: divert water away from rills or solve rill erosion

(4.3) NOT FINISHED

(4.4) Earth’s Atmosphere

  • (4.4) Earth’s Atmosphere(4.4) Earth’s AtmosphereAtmosphere contains:

    • Nitrogen (78%)

    • Oxygen (21%)

    • Trace Gases (1%)

      • Argon → Carbon dioxyde → Neon → Helium → CH4 → Krypton → Hydrogen → Water

  • Atmosphere layers

    • Exosphere (600-10,000 km)

      • enters space → drop in temperature

    • Thermosphere (85-600 km)

      • x-ray radiation + UV rays → rise in temperature

      • air’s still thin

    • Mesosphere (50-85 km)

      • thinning atmosphere → drop in temperature

    • Stratosphere (20-50 km)

      • radiation → rise in temperature

    • Troposphere (0 to 6-20 km) 

      • varies depending on location

      • densest layer

      • contains weather

(4.5) Global Wind Patterns

  • Earth’s rotation → air circulates → predictability of wind patterns

    • Causes different ecosystems 

      • EX: Tropical climates near the equator

  • Convection: cycle caused by earth’s rotation

    • as air expands, gets less dense and moves up to the poles → air heats,

    • as air compacts, gets denser and returns down → air cools down

    • repeats

    • exemplified in a Hadley Cell

Schematic of the Hadley circulation. Abbreviations: TTL-Tropical... |  Download Scientific Diagram
  • Coriolis Effect: Earth deflecting winds as it rotates 

    • Hot air from equator deflects → colder air

(4.6) Watersheds

  • Watershed: area of land that drains water into a central body of water

    What is a Watershed? — AQUETONG WATERSHED ASSOCIATION
    • Highest point/divide: highest point of watershed

    • Tributary: where water runs down from highest point

      • Transition zone

    • River: more water comes down

      • Transition zone

    • Delta: rivers join and water falls into basin (aquifer)

    • Groundwater/aquifer: the basin which has the runoff

  • Characteristics of watersheds:

    • Area

    • Vegetation

      • More vegetation = water is absorbed in the soil → groundwater

    • Type of soil

      • Permeable soil = water in groundwater

      • Impermeable soil = runoff

    • Slope 

      • Steeper = runoff than absorb into the ground

  • Human activity that affect watershed

    • Logging (removal of trees → sediment of soil runs in water)

    • Industrial sites (pollution → rivers)

    • Residential areas (waste, usage → quality or amount of water)

    • Cities (water runs off of streets)

    • Livestock/cropland (fertilizers + pesticides → quality of water)

    • Dams (blocks sediments that goes into natural habitats)

(4.7) Solar Radiation + Earth’s Seasons

  • Insolation: how much solar radiation areas of Earth recieves 

    • Equator gets more concentrated insolation, poles get less (sun reaches farhter)

    • Solar radiation can get scattered over atmosphere

  • Seasons happen because of Earth’s tilt, NOT Earth’s faces

    • Affects equinoxes, solstices, poles’ hottest/coldest days, 

      • EX: tropic of crapicorn = most solar radition during December, tropic of cancer = most solar radiation in June

(4.8) Earth’s Geography + Climate

  • Air moves over water → water evaporates → air heats up

  • Air continues to land → water condenses → cools down → falls (snow, rain, etc)

    • As it continues, air is less dense and gets slightly warmer

  • Rain-shadow effect: how air moisture changes as air comes from the sea → mountain → land

    • Water evaporates with air over ocean → rises up the mountain on windward side (precipitation through rain) → condenses + cools down → less dense as it drops in leeward side

    • Windward side: side of a mountain facing coastline

    • Leeward side: side of a mountain facing inland

      • Arid climate because of effect

(4.9) La Niña + El Niño

  • ENSO (El Niño Southern Oscillation): drastic extremes between El Nino, La Nina, and normal ocean circulation petterns

    • El Niño = hot, La Niña = cold

    • Takes place in equator

  • Normal circulations

    • Trade winds bring warm temperatures from east to west 

      • Brings more wind and rainfall to Australian + Southeast Asia region 

      • Upwelling (cold, nutrient + oxygen rich water moves to the surface to replace warm waters blown away) in the Americas

      • Thermocline tilts from east to west (rises in east, lowers in west)

  • El Niño 

    • Flips wind patterns

      • No upwellign and warmer water in Americas

      • Colder, drought conditions in Australia region

        • Flooding since region isn’t used to that much water

      • Thermocline levels

  • La Niña

    • Extreme version of normal circulations, strong trade winds

      • Flash flooding in Australia region

      • Drier climate in Americas

      • More upwelling in Americas → more nutrient + oxygen rich water

      • Thermocline is steep