Continental Drift
Proposed by Alfred Wegener (1915)
🌍 Pangaea: A supercontinent that began breaking apart 200 million years ago.
🔍 Evidence for Continental Drift:
1⃣ Fossils of extinct land animals on separate continents.
2⃣ Fossilized tropical plants under Greenland’s ice caps.
3⃣ Glaciated landscapes in the tropics (Africa & South America).
4⃣ Rock similarities between America’s east coasts and Africa & Europe’s west coasts.
5⃣ Continents fit together like puzzle pieces.
6⃣ Past polar climates in tropical regions (paleo-climatic data).
Seafloor Spreading Theory (1960s)
🌊 Key Discoveries:
Alternating magnetic patterns in oceanic rocks.
Rocks near mid-ocean ridges are younger; older farther away.
Suggests new crust is formed at volcanic rift zones.
Lithosphere & Plate Movement
🌍 The lithosphere is the solid outer layer of Earth.
🛑 Plates move slowly, causing earthquakes and volcanoes.
🔽 Subduction Zones:
Areas where one tectonic plate moves under another.
Causes volcanoes and earthquakes.
1⃣ Convergent Boundaries (➡⬅)
Plates move toward each other.
Creates:
Subduction zones (one plate moves under another).
Orogenic belts (if plates collide and compress).
Example: Cascade Mountain Range.
🔽 When Oceanic & Continental Plates Converge:
Denser oceanic plate subducts beneath the continental plate.
Forms oceanic trenches & mountain ranges.
🏝 When Two Oceanic Plates Converge:
Forms an island arc (volcanic islands).
A deep-sea trench forms at the subduction zone.
🏔 When Two Continental Plates Converge:
Mountain ranges form as plates compress & push up.
2⃣ Divergent Boundaries (⬅➡)
Plates move apart.
Forms fault zones & oceanic ridges.
Frequent earthquakes occur.
🌊 Examples:
Mid-Atlantic Ridge (Oceanic Divergent Boundary).
East African Great Rift Valley (Continental Divergent Boundary).
3⃣ Transform Boundaries (⬆⬇)
Plates slide past each other in opposite directions.
Friction & stress buildup cause earthquakes.
Example: San Andreas Fault.
Soil
🟤 Definition: A thin layer on Earth’s land surface that is a basic natural resource, affecting ecosystems.
🔹 Main Ingredients:
1⃣ Minerals of different sizes.
2⃣ Air & water in open spaces.
3⃣ Organic material from decomposed plants & animals.
Soil Profile (Layers of Soil)
🌿 O Horizon (Surface Litter)
Leaves & decomposing debris on top.
🌱 A Horizon (Topsoil)
Organic matter, living organisms, inorganic materials.
Thickest in grasslands.
⬇ E Horizon (Zone of Leaching)
Dissolved & suspended materials move downward.
🟡 B Horizon (Subsoil)
Yellowish due to iron, aluminum, humic compounds, and clay from A & E horizons.
⛰ C Horizon (Weathered Parent Material)
Partially broken-down rock & minerals.
Factors Affecting Soil Formation
🌦 Climate
Precipitation & temperature affect the weathering of parent material.
🦠 Living Organisms
Bacteria (Rhizobium), fungi, insects, worms, snails help break down organic matter.
🪨 Parent Material
The original rock & minerals that soil forms from.
Can be native or transported by wind, water, glaciers.
🏔 Topography
Land shape & elevation influence soil formation.
Soil Erosion
🌍 Definition:
The movement of weathered rock/soil due to water, wind, or human activity.
⚠ Effects:
Reduces water-holding capacity.
Destroys soil profile.
Increases soil compaction.
🚜 Poor Agricultural Practices That Cause Erosion:
❌ Improper plowing.
❌ Monoculture (planting only one crop).
❌ Overgrazing.
❌ Removing crop waste instead of returning it to the soil.
Landslides & Mudslides
🏔 Landslides
Masses of rock, earth, or debris move down a slope.
Can be triggered by heavy rain, droughts, earthquakes, volcanic eruptions.
🌊 Mudslides (Debris Flows)
Fast-moving landslides that flow in channels.
Begin on steep slopes and are worsened by wildfires or construction.
🌍 High-Risk Areas:
✅ Places with previous landslides.
✅ Locations with high surface runoff.
✅ Steep slopes or areas near rivers & canyons.
Rock Types
🔥 Igneous Rocks (Formed by cooling lava/magma)
Intrusive: Cools slowly underground, large-grained.
Extrusive: Cools quickly on surface, fine-grained.
Weathering & water transport break them down.
🌋 Metamorphic Rocks (Formed by heat & pressure)
Examples: Diamond, marble, slate, anthracite coal.
🪵 Sedimentary Rocks (Formed by layers of compacted materials)
Only rock type that contains fossils.
Soil Components
🪨 Gravel
Coarse particles made of rock fragments.
🏖 Sand
Larger than silt, high permeability (water drains too quickly).
Good for crops needing less water.
🌾 Loam
Balanced mix of clay, sand, silt, & humus.
Rich in nutrients & holds water without waterlogging.
💦 Silt
Fine sediment between sand & clay in size.
Easily transported by water.
🌑 Clay
Very fine particles, compacts easily.
Low permeability, leading to waterlogging.
🌱 Humus
Dark organic material from decayed plants & animals.
Improves soil structure, aeration, & pH stability.
Mixed by earthworms.
Components of Soil Quality
💨 Aeration
Refers to how well soil absorbs oxygen, water, & nutrients.
Helps root growth & reduces soil compaction.
🧱 Soil Compaction
Highly compacted soil has few large pores, reducing water infiltration & drainage.
🌾 Nutrient-Holding Capacity
Ability to retain & provide nutrients for plants.
Weathering releases nutrients, but leaching can reduce soil fertility.
Key nutrients: Nitrogen (N), Phosphorus (P), Potassium (K).
💧 Permeability
How well water & oxygen pass through soil.
Low permeability can cause salinization.
🧪 pH Levels
Acidic soil → caused by acid rain, pollution, or high rainfall.
Alkaline soil → contains high potassium (K), calcium (Ca), magnesium (Mg), or sodium (Na).
🌿 Pore Size
Determines how much water, air, & nutrients reach plant roots.
💧 Water-Holding Capacity
Controlled by soil texture & organic matter.
Fine soils hold more water, coarse soils drain faster.
🌍 Soil Texture
Defined by particle size distribution.
Affects moisture, nutrients, & oxygen retention.
🌱 Soil Food Web
Community of organisms that live in soil.
Affects nutrient cycling, plant health, & soil structure.
🌍 Greenhouse Effect & Early Life
CO2 (volcanoes) & CH4 (early microbes) → Strong greenhouse effect enabled life to develop.
💨 Great Oxidation Event (GOE) (2.5 BYA)
Oxygen rise → killed most life on Earth.
Methane (CH4) → oxidized into CO2, weakening the greenhouse effect, leading to cooling & ice ages.
Higher O2 → biological diversification & chemical changes in atmosphere, oceans, and rocks.
Atmosphere’s Current Composition
🟡 Nitrogen (N2) - 78%
Key nutrient for organisms (in amino acids & nucleic acids).
Enters the atmosphere through denitrification & combustion.
🟢 Oxygen (O2) - 21%
Vital for respiration & produced in photosynthesis.
Became abundant 2.5 billion years ago.
💦 Water Vapor (H2O) - 0-4%
Highest near the equator & oceans, lowest in polar & desert regions.
Sources: evaporation, respiration, combustion, volcanoes, transpiration.
🌫 Carbon Dioxide (CO2) - <1%
Produced by respiration, fossil fuel combustion, & decay.
Absorbed in photosynthesis.
Major greenhouse gas, lifespan ~100 years.
Atmosphere’s Structure
☁ Troposphere (0–10 km / 0–6 mi)
75% of atmosphere’s mass & almost all water vapor.
Weather occurs here.
Temperature & pressure decrease with height.
☀ Stratosphere (10–50 km / 6–30 mi)
Ozone (O3) absorbs UV radiation.
Temperature increases with altitude.
🌦 Weather
Caused by heat energy transfer from unequal solar heating.
Includes: Air pressure, temperature, humidity, precipitation, wind speed/direction, sunlight.
🌍 Climate
Long-term weather patterns (months to millions of years).
Controlled by latitude, altitude, ocean distance, albedo, & human activity.
🔥 Convection
Main energy transfer process.
Warm air rises, creating wind & pressure differences.
🌡 Heat Index (HI)
Feels like temperature with humidity factored in.
🌪 Air Mass
Large body of air with similar temperature & moisture.
Types: Equatorial, tropical, polar, Arctic, continental, maritime.
☀ Albedo
Reflectivity of a surface.
High albedo: Ice & snow.
Low albedo: Oceans & dark land.
🌊 Oceans & Temperature Stability
Water heats/cools slowly compared to land.
Coastal areas have less extreme temperature changes than inland.
🌡 Fronts (Boundary Between Air Masses)
Cold Front → Thunderstorms & strong winds.
Warm Front → Gradual warming & light rain.
Stationary Front → Lingering weather patterns.
🌿 Greenhouse Effect
Keeps Earth warm, but excess traps heat → Global warming.
Main greenhouse gases: H2O, CO2, CH4, N2O.
🏙 Human Activity & Climate
Pollution increases rainfall in urban areas.
Deforestation & urbanization impact climate.
🌍 Latitude & Sunlight
Farther from equator = Less sunlight.
Poles receive spread-out solar energy.
💨 Moisture Content of Air
Determines plant growth, biome type.
🌫 Pollution & Greenhouse Gases
Emitted from natural & human sources.
🌎 Earth’s Rotation & Temperature
Day/Night cycle affects daily temperature patterns.
🌋 Volcanoes & Climate
Sulfur-rich eruptions → Cooling & stratospheric warming.
Volcanic aerosols last 1–3 years & can damage ozone layer.
🌬 Land Breeze (Night)
Land cools faster than the sea.
Denser air over land moves to sea.
🌊 Sea Breeze (Day)
Land heats up faster than the sea.
Less dense air over land rises, and cooler sea air moves in.
🔄 Air Circulation
Warm air rises due to Earth's rotation, revolution, and tilt.
Cool air sinks, creating convection & winds.
🌪 Low-Pressure Systems
Lower pressure at center.
Air rises, forms clouds & precipitation.
🌞 High-Pressure Systems
Higher pressure at center.
Winds blow outward.
Clockwise in Northern Hemisphere, counterclockwise in Southern Hemisphere.
Associated with fair weather.
💨 Trade Winds
Easterly surface winds in the tropics.
Used by sailing ships for navigation.
🌬 Wind Speed & Direction
Higher pressure difference = Higher wind speed.
Easterly winds come from the east.
Westerly winds come from the west.
🌍 Coriolis Effect
Earth's rotation curves wind paths.
Northern Hemisphere: Winds spiral clockwise out from high pressure & counterclockwise toward low pressure.
Hadley Air Circulation
🔥 Near the Equator
Warm air rises, spreads north & south.
High humidity, heavy rainfall → Rainforests.
🏜 Subtropical Regions
Air cools, sinks, & becomes dry.
Low humidity, little cloud formation → Deserts.
☀ Climate Characteristics
Warm to hot summers, mild winters.
Savanna climate has a dry season over two months long.
🌍 Ferrel Cells (30°–60° latitude)
Mid-latitude climates → Defined seasons.
Severe winters & cool summers due to cyclone patterns.
❄ Polar Cells (Above 60° latitude)
Cold, dry air sinks → Polar deserts.
Little precipitation because water is frozen.
🌪 Polar Vortex
Low-pressure zone over poles with cold air.
Strengthens in winter, weakens in summer.
Antarctic vortex linked to ozone depletion.
🌊 Hurricanes (Cyclones/Typhoons)
Over warm oceans where trade winds converge.
Rotating thunderstorms absorb ocean moisture & heat.
Eye → Low pressure, descending air.
Storm surge → Sea level rise during storm.
🌪 Tornadoes
Updrafts & downdrafts create a rotating mesocyclone.
Warm air rises, cold air sinks, forming a funnel
🌧 Monsoons
Seasonal winds changing direction.
Winter: Blow from land to sea (dry season).
Summer: Blow from sea to land (wet season).
💧 Watershed
A land area that drains rainfall & snowmelt into a lake, ocean, or aquifer.
🌊 Mississippi River Watershed
Largest watershed in the U.S.
Drains over 1 million square miles.
🌱 Watershed Management
Reduces pesticides & fertilizers from washing into waterbodies.
Uses land, forest, and water resources responsibly.
Protects plants, animals, and water quality.
☀ Angle of Sunlight
Heat energy received depends on the sunlight's angle.
Varies by location, time of day, & season.
Tilt of Earth's axis causes seasonal changes.
Lower angle = Weaker sunlight spread over a larger area.
🌍 Solar Intensity Factors
Tilt of Earth’s axis (23.5°).
Atmospheric conditions.
Earth’s yearly orbit around the sun.
Earth’s 24-hour rotation on its axis.
🌊 Bodies of Water and Climate
Over 70% of Earth's surface is covered in water.
Oceans & lakes store heat, adding moisture to air, driving air currents.
Water stabilizes climate by absorbing heat in warm periods & releasing in cooler ones.
Warm, moist ocean air drives precipitation patterns when carried over land.
🏞 Higher Elevations = Cooler Climates
Elevation increases = cooler climates and longer cold seasons.
Lower air pressure at higher elevations = cooler temperatures.
High-altitude plains are deserts due to being downwind of mountains.
📏 Latitude and Tropics
Latitude measures distance from the equator.
Tropic of Cancer = northernmost latitude of overhead sun.
Tropic of Capricorn = southernmost latitude of overhead sun.
🏔 Mountains and Air Flow
Mountains act as barriers to air currents.
Air cools & rains on windward side, creating a rain shadow effect on leeward side.
Rain shadow affects plant & animal life on the leeward side.
🌊 La Nada (Normal Conditions)
Easterly trade winds push water & air west.
Western Pacific has warmer water (14°F) & higher ocean (24 inches).
Upwelling brings nutrient-rich water to the surface.
🔥 El Niño (Warm Phase)
Air pressure patterns reverse, weakening trade winds.
Water piles up in the western Pacific, weakening upwelling.
Warmer-than-average ocean temperatures occur off South America.
Jet stream changes, increasing ocean warmth & affecting weather.
❄ La Niña (Cool Phase)
Stronger trade winds push cooler water west, increasing upwelling.
Cooler-than-normal ocean temperatures off South America.
Wetter-than-normal in Pacific Northwest & drier in southern US.
More hurricanes & cooler winters in southeast US.
🌎 Environmental Effects of ENSO Patterns
Warmer/cooler ocean temperatures disrupt marine ecosystems.
Decrease in upwelling = fish die-offs & negative effects on coral reefs.
Changes in weather increase insect-borne diseases & migration patterns.
Hurricanes & tornadoes become stronger & more frequent.
Altered ocean currents & glacial melting with warmer oceans.
Flooding and soil erosion with increased rainfall.