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Visual Review
AP Environmental Science Unit 4 Visual Review
A 9-slide visual walkthrough of every Topic 4.1-4.9 concept — plate tectonics, soil, the atmosphere, global wind patterns, watersheds, seasons, climate, and El Niño/La Niña — built right into the page.
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TOPIC 4.1
Plate Tectonics
CONVERGENT (collision)
DIVERGENT (spreading)
TRANSFORM (sliding)
Three boundary types, three outcomes
Convergent — plates collide, forming mountains (or subduction zones with volcanoes/earthquakes).
Divergent — plates pull apart, magma rises to form new crust (mid-ocean ridges, rift valleys).
Nearly every major mountain range, volcano belt, and earthquake zone sits on a plate boundary.
The Review Hub · AP Environmental Science Unit 4
TOPIC 4.2
Soil Formation and Erosion
O — organic litter
A — topsoil (humus)
B — subsoil
(mineral accumulation)
C — weathered rock
R — bedrock
How soil forms
Four factors, working over centuries:
Parent rock weathers physically & chemically.
Climate (temp/moisture) speeds weathering.
Organisms add organic matter & mix layers.
Time — soil takes centuries to build, years to lose.
Erosion strips it away
Wind and water carry away exposed topsoil —
worsened by deforestation, overgrazing, and
tilling that leaves soil bare. Contour plowing,
terracing, and cover crops slow it down.
The O and A horizons hold nearly all the nutrients — lose those, and the field's fertility is gone for generations.
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TOPIC 4.3
Soil Composition & Properties
CLAY
SAND
SILT
loam
% sand / silt / clay determines the texture class
Texture: particle size mix
Sand (largest) drains fast, holds little water.
Clay (smallest) holds water & nutrients, but
drains poorly and compacts easily.
Loam — the balanced mix — is ideal for farming.
Porosity vs. permeability
Porosity — the total space BETWEEN particles
(how much water/air it can hold).
Permeability — how easily water moves
THROUGH those spaces. Clay can be porous but
impermeable — tiny, disconnected pores.
Loam's balance of sand, silt, and clay makes it the most agriculturally productive texture class.
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TOPIC 4.4
Earth's Atmosphere
Troposphere
Stratosphere
(ozone layer)
Mesosphere
Thermosphere
surface
↑ altitude
Composition
78% nitrogen (N₂), 21% oxygen (O₂), <1%
argon and trace gases — including CO₂ and
other greenhouse gases that trap heat and
regulate Earth's temperature.
The layer that matters most
Nearly all weather happens in the
troposphere — the thin bottom layer. The
stratosphere above it holds the ozone layer,
which absorbs harmful UV radiation.
Temperature actually rises with altitude in the stratosphere — the opposite of the troposphere below it.
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TOPIC 4.5
Global Wind Patterns
equator
Hadley
Hadley
Ferrel
Ferrel
warm air rises at equator, sinks near 30° N/S
Why the cells exist
The equator receives more direct sunlight than
the poles. Warm equatorial air rises, cools, and
sinks around 30° latitude — creating the
Hadley, Ferrel, and Polar circulation cells.
The Coriolis effect
Earth's rotation deflects moving air — right in
the Northern Hemisphere, left in the Southern.
This bends straight north-south airflow into the
trade winds and westerlies we actually observe.
Deserts cluster near 30° N/S latitude because that's exactly where the sinking, dry Hadley-cell air lands.
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TOPIC 4.6
Watersheds
watershed boundary (divide)
outlet (lake/river)
Definition
A watershed is all the land area that drains
into a single body of water. It's bounded by a
divide — a ridge of higher elevation.
Every point on Earth belongs to some watershed.
Land use anywhere affects the outlet
Fertilizer, pesticides, and sediment from ANY
point in the watershed can wash downstream
to the outlet — this is why a farm miles from a
lake can still cause the eutrophication seen
in Topic 1.6.
Impervious surfaces (roads, parking lots) shrink infiltration and speed runoff straight to the outlet.
The Review Hub · AP Environmental Science Unit 4
TOPIC 4.7
Solar Radiation and Earth's Seasons
sun
N tilted toward sun
(N summer)
N tilted away
(N winter)
Why seasons happen
Earth's axis is tilted about 23.5°. As Earth orbits the sun, that fixed tilt points different hemispheres
toward the sun at different times of year — NOT distance from the sun, which barely changes.
More direct sunlight AND longer days both follow from the same tilt — that's why summer days feel endless.
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TOPIC 4.8
Earth's Geography and Climate: Rain Shadow
moist ocean air
rain on windward side
dry descending air
desert (rain shadow)
Four regional shapers
Latitude — sets baseline temperature.
Elevation — higher = cooler, thinner air.
Ocean currents — warm/cool coastlines.
Rain shadow — mountains force air up,
it cools, drops moisture on the windward
side, then descends dry on the leeward side.
Classic example: the Sierra Nevada creates
California's Death Valley rain shadow desert.
Same storm, two outcomes: lush forest on the windward slope, desert just miles away on the leeward side.
The Review Hub · AP Environmental Science Unit 4
TOPIC 4.9
El Niño and La Niña
NORMAL CONDITIONS
trade winds →
warm water piles up (west)
cold upwelling (east)
EL NIÑO
weakened winds
warm water shifts east — no upwelling
ENSO — a Pacific-wide seesaw
El Niño: trade winds weaken, warm water spreads east, cutting off the cold upwelling that normally feeds Pacific fisheries.
La Niña is the reverse: stronger trade winds, cooler eastern Pacific, intensified upwelling and normal patterns exaggerated.
El Niño years often mean fewer fish off South America — the upwelling that feeds them briefly shuts off.
The Review Hub · AP Environmental Science Unit 4
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How to use the visual review
Spend 30 seconds per slide before clicking next. Look at the diagram, then ask yourself: "Could I draw this from memory and explain it?"
Use the fullscreen button () on desktop for the best experience. Use arrow keys to navigate. Tap "Show all slides" to jump around.
This covers every one of Unit 4's 9 CED topics, from plate tectonics through the El Niño Southern Oscillation.