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Flashcards covering key vocabulary from geography lecture notes, including Earth structure, plate tectonics, volcanoes, earthquakes, fold mountains, rock cycle, weathering, mass movement, rivers, coastal landscapes, glacial landscapes, and soils.
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Crust
Outermost layer of the Earth made of solid rock, broken into tectonic plates.
Mantle
Layer beneath the crust, mostly solid with semi-molten rock (magma), moves in convection currents.
Core
Center of the Earth, made of iron and nickel, with a liquid outer core and solid inner core.
Convection Currents
Large currents of hot magma that move in circles inside the mantle, pushing and pulling Earth’s plates.
Plate Tectonics
Idea that the Earth's crust is broken into big pieces called plates that move because of convection currents in the mantle.
Continental Drift
German scientist Alfred Wegener's idea that all continents were once joined in a supercontinent called Pangaea and drifted apart over time.
Seafloor Spreading
Process where plates separate under the ocean, with molten magma coming to the surface to form new crust.
Continental Plates
Carry land.
Oceanic Plates
Located under the sea.
Plate Boundaries
The edges where plates meet.
Constructive Plate Boundary
Plates move apart.
Destructive Plate Boundary
Plates move towards each other.
Conservative Plate Boundary
Plates move side by side.
Rift
Crack where magma comes to the surface at a constructive plate boundary.
What Forms at Constructive Boundaries?
Volcanoes, volcanic islands, mid-ocean ridges, and earthquakes.
Subduction
Oceanic plate sinks under continental plate, forming fold mountains and volcanoes.
Volcano
A volcanic mountain formed when magma moves up to the Earth's surface through a vent.
Crater
Opening where magma erupts out of the vent.
Lava
Hot magma on Earth's surface.
Active Volcano
Erupts regularly or likely to erupt.
Dormant Volcano
Hasn't erupted in some time.
Extinct Volcano
Has not erupted in historic times.
Pacific Ring of Fire
Zone of active volcanoes and earthquakes around the edge of the Pacific Ocean.
Geysers
Shoot hot water into the air when underground water is heated by magma.
Positive Economic Impacts of Volcanoes
Tourism and recreation, heating and electricity, agriculture and fish farming.
Positive Social Impacts of Volcanoes
Clean fuel source improving air quality and reducing climate change impact.
Earthquake
Sudden shaking of the Earth's surface when two plates collide or slide past each other.
Focus
The spot underground where plates slip and the earthquake starts.
Epicenter
Spot on the surface directly above the focus.
Tsunami
Giant wave caused by strong underwater earthquakes.
Fault
Crack in the Earth where plates get stuck.
Seismograph
Machine used to record and measure earthquakes.
Richter Scale
Measures how strong an earthquake is on a scale of 1 to 10.
Mercalli Scale
Measures the damage caused by an earthquake based on what people see and feel.
Short-Term Responses to Volcanoes
Evacuations, emergency aid, rescue teams, and medical help.
Long-Term Responses to Volcanoes
Rebuilding homes and infrastructure, monitoring volcanoes, education and planning.
Predicting (Earthquakes)
Guessing earthquake-prone areas based on ground movement, radon gas, and animal behavior.
Planning (Earthquakes)
Reducing earthquake damage by stopping building on fault lines and making buildings stronger.
Preparation (Earthquakes)
Earthquake drills and training rescue teams.
Anticlines
Long ridges that form mountains when tectonic plates collide.
Synclines
Valleys between the ridges.
Ireland's Fold Mountain History
The Caledonian Mountains, Armorican Mountains, and Alpine Mountains.
Rock Cycle
Atoms make up elements, which combine to form minerals; minerals combine to form rocks.
Igneous Rocks
Form when magma or lava cools.
Sedimentary Rocks
Form when rocks break down into sediments that are buried and pressed together.
Metamorphic Rocks
Form when heat and pressure change igneous or sedimentary rocks.
Granite
Forms when magma cools slowly inside the Earth's crust, grey with speckles, hard and rough texture.
Basalt
Forms when lava cools quickly on the Earth's surface, dark-grey or black, hard and smooth texture.
Limestone
Formed from dead sea creatures, sand, and shells that built up on the sea floor.
Sandstone
Made from sand layers that were compacted and cemented by silica on the ocean floor.
Marble
Formed when heat from magma changes limestone.
Quartzite
Formed when sandstone is changed by heat from magma.
Drilling
Used to get oil and gas from underground or under the sea.
Opencast Mining/Quarrying
Used when resources are near the surface; cheapest method, but creates noise and damages landscapes.
Shaft Mining
Used for resources deep underground, like coal and metal ores; expensive, dangerous, and damages the land.
Resource Uses
Stone, sand, and gravel for building materials; coal, oil, and gas for energy; metals and precious stones.
Consequences of Rock Exploitation
Impacts due to tailing leaking into waters, effects landscapes visually- reduces CO₂ emission
Weathering Definition
A process that affects rocks that causes them to be broken into smaller pieces over time.
Mechanical (Physical) Weathering
Breakdown of rock without changing its chemical composition.
Chemical Weathering
Breakdown of rock through chemical reactions (Carbonation).
Carbonation
Rainwater absorbs CO₂, forming carbonic acid that dissolves limestone.
Biological Weathering
Breakdown of rock by living organisms (tree roots, burrowing animals, lichens).
Erosion Definition
The removal of rock and soil by moving agents such as water, wind, ice or biological activity
Swallow Holes
Streams disappear underground.
Stalactites
Hang from the ceiling (from dripping water losing CO₂ and depositing calcite).
Stalagmites
Build up from the floor beneath stalactites.
Mass Movement
Movement of loose, weathered material downslope due to gravity.
Types of Mass Movement
Soil Creep, Landslide, Bog Burst, Mudflow.
Bog Burst (Bog Slide)
Peat becomes saturated and slides down hills, destroying everything in its path.
Landslides
Over Saturation of Soil causing fast movement of rock/soil.
Preventing Mass Movement
Terracing/Benching (flattens slopes), Anchor Bolts, Geomesh, Concrete Walls, Metal Sheet Piles, Drainage, Planting Trees.
River
A body of water that flows in a channel, shaping the landscape.
River Processes
Erosion, Transportation, Deposition.
Hydraulic Action
Water hits the riverbanks and bed with force, breaking pieces away.
Attrition
Rocks and stones hit each other and break into smaller, smoother pieces.
Abrasion
Stones carried by the river scrape and wear away the riverbed and banks.
Solution
Water dissolves certain types of rock, like limestone.
Rolling (Traction)
Big stones roll along the riverbed.
Bouncing (Saltation)
Small stones and sand bounce along the bottom.
Suspension
Fine particles like silt and clay float in the water.
Solution
Dissolved materials (like salts) are carried invisibly in the water.
V-Shaped Valley
Narrow valley with steep sides.
Interlocking Spurs
High ground jutting out on either side of river.
Meanders
Large bends in a river.
Levees
Raised ridges beside riverbanks.
Deltas
Triangular area of land at a river mouth.
Dams
Concrete wall across a river to control flow or create energy, forming a reservoir.
Waves
ripples on the sea, caused by wind.
Swash
Water that rushes up the beach after a wave breaks.
Backwash
Water that flows back down the beach.
Coastal Defenses
Groynes, rock armour, seawalls and gabions
Tombolos
Sand/shingle ridge connecting an island to the mainland.
Groynes
Walls made from wood or concrete, built at right angles to the shore to trap sand.
Rock Armour (Boulders)
Big rocks placed at the base of cliffs or dunes to absorb wave energy.
Sea Walls
Strong walls built at the back of beaches, often curved to reflect waves back into the sea.
Gabions
Wire cages filled with stones, placed in front of dunes or at the back of beaches to absorb wave energy.
Glaciation
Earth has experienced periods of much colder climate.
Plucking
Ice melts, enters cracks, refreezes, sticks to rock, moving glacier pulls out the rock.
Abrasion
Plucked rocks at glacier’s base scrape the ground, acting like sandpaper, leaves striations.
Moraines
Long ridges of unsorted, loose rock left behind as landforms of deposition after glaciers melt.