Utilisateur
a naturally occurring event that poses a threat to people, property or the environment
Tectonic
Climatic
- Frequency
- Population density
- Urbanisation
- Climate change
Earth's outer layer, the lithosphere, is broken into large, rigid plates that move relative to eachother
- Older, lighter and cannot be destroyed
Denser, can be subducted and is constantly being destroyed and replaced at plate boundaries
In similar places in narrow zones of activity. These zones include:
- The Pacific Ring of Fire
- The Mid-Atlantic Ridge
- Southern Europe
Where over 450 of the world's active and dormant volcanoes are located, and where about 90% of all earthquakes happen
- The plates move towards one another which can cause earthquakes and volcanoes
- As the plates collide, the oceanic plate is forced beneath the continental plate (this is known as subduction) and results in the formation of an ocean trench
- When the plate sinks into the mantle it melts to form magma.
- The pressure of the magma builds up beneath Earth's surface
- Th magma escapes through a composite volcano and erupts violently
- The plates are moving apart from one another
- The magma in the mantle rises up to make a new crust
-The movement of plates over the mantle can cause earthquakes
- Rising magma can also create shield volcanoes
- The plates slide past each other in opposite directions, or in the same direction at different speeds
- As the plates try and move, friction occurs and the plates become stuck
- Pressure builds up because the plates are still trying to move
- When pressure is released it sends out huge amounts of energy, causing an earthquake
- Volcanic ash results in fertile soil
- Availability of geothermal energy
- Lower house prices
- Sentimental value
- Sulfur extraction from volcanoes
Regions on Earth's surface characterized by either high or low atmospheric pressure, which influences weather patterns and wind circulation
Tropical storms primarily occur in tropical regions between 5 and 30 degrees north and south of the equator
This is a major circulation pattern in the tropics where warm, moist air rises, cools, condenses and creates the low pressure zone of the ICTZ
This is a belt of low pressure around the equator where trade winds from the north and south converge, causing uplift and heavy rainfall
The trade winds, which blow from subtropical high-pressure zones towards the equator, are a key component of the Hadley cell and provide the initial impetus for the formation of tropical storms
This effect, caused by Earth's rotation, deflects the rising air, creating a swirling motion that initiates the rotation of tropical storms
A combination of:
- Warm ocean water: provides energy and moisture for the storm
- Low wind shear: allows the storm to intensify
- The Coriolis effect: gives the storm its spiral shape
1. Warm ocean water (at least 27 degrees celcius) heats the air above it, causing it to rise rapidly creating an area of low pressure
2. Air from surrounding areas rushes in to fill the space left by the rising air, leading to strong winds
3. As the rising air continues to climb, it cools and the water vapor condenses into clouds, releasing latent heat
4. The cumulonimbus clouds become large and release heat, further driving the storm
5. The coriolis effectt occurs, forming a cyclone
6. In the center, cold air sinks, creating a calm, clear area known as the eye of the storm
- Warmer ocean temps meaning more succeptability to the formation of tropical storms in areas they were previously uncommon
Satellites and radar systems track the formation, movement and intensity of tropical storms, providing real-time data
Computer models use data from monitoring to predict the storm's path, allowing for early warnings and evacuation plans
- Building Codes: Enforcing strict building codes ensures structures can withstand high winds and flooding
- Coastal defences: Sea walls, levees and storm surge barriers protect coastal communities
- Reinforced structures: Strengthening windows, doors and roofs reduced damage from flying debris
- Evacuation plans: Well-coodinated evacuation plans ensure safe and efficient displacement of people
- Disaster supply kits: Preparing essentials like food, water and first-aid kits ensures preparedness
- Community awareness: Education and training programs inform residents about storm risks and appropriate actions
- Rain
- Wind
- Heatwaves
- Thunderstorms
- Hailstorms
- Snow
- A rise in average temperatures
- Increased intensity of extreme weather events like heatwaves and storms
- Shifts in percipitation patterns including drier summers and wetter winters
- Natural factors: orbital changes, volcanic activity and solar output
- Human factors: use of fossil fuels, agriculture and deforestation
1. Glacial-interglacial cycles: Repeated periods of cold and warm periods which have dramatically altered sea levels, landscapes and ecosystems
2. Rapid warming and sea level rise: Following the last glacial period, Earth experienced a rapid warming which caused sea levels to rise leading to flooding and the formation of coastal features
3. Modern climate change: Human activities have led to a rapid increase in greenhouse gas concentration in the atmosphere resulting in global warming
Mitigation - reducing causes
Adaptation - responding to change
- Mitigation: renewable energy production, carbon capture, planting trees and international agreements
- Adaptation: change in agricultural systems, managing water supply, reducing risk from rising sea levels
- The foundation of an ecosystem
- Use photosynthesis to convert energy into food (self-feeders)
- They obtain energy by consuming producers or other consumers
- E.g. herbivores, carnivores, omnivores
- Decomposers like fungi and bacteria break down dead organic matter including dead plants and animals
- They recycle nutients back into the environment making them available for producers to use
- The continuous movement of nutrients through an ecosystem
- These cycles include the carbon cycle and the nitrogen cycle
- High average temp
- Substantial rainfall
- Nutrient-poor soils
1. Commercial farming
2. Logging
3. Road building
4. Mineral extraction
5. Population growth
1. Economic development
2. Soil erosion
3. Contribution to climate change
By preserving more of the forest's structure and allowing for faster recovery compared to clear-cutting. It involves only removing less valuable trees, leaving behind younger ecologically important trees.
Creates a sustainable financial incentive for conservation. Ecotourists:
- Travel in small groups
- Keep to footpaths
- Don't leave litter
- Don't start fires
1. Mineral extraction
2. Energy from heat (thermal)
3. Farming
4. Tourism
1. Extreme tempertures
2. Limited water supply
3. Inaccessibility to deserts
1. Climate change
2. Overgrazing
3. Over-cultivation
4. Soil Erosion
1. Water and soil management
2. Tree planting
3. Use of appropriate technologies
Transverse and longitudinal
- Definition: The water oscillates up and down as the wave travels horizontally
- Components: Crests and troughs
- Examples: Water waves, ripples on a pond
- Definition: The air vibrates back and forth as the wave travels in the same direction
- Components: Areas of low pressure and areas of high pressure
- Examples: Seismic waves
- Rocks are broken down by forces like freeze-thaw cycles
Rocks are dissolved or changed by chemical reactions, often with rainwater or seawater
Large blocks of material slide downhill, often due to gravity
Saturated soil or rock slumps down a curved surface
Pieces of rock detach from a cliff face and fall down, often due to weathering weakening the rock
The force of waves crashing against a cliff can compress air in cracks, weakening the rock and causing it to break
Waves carrying sediment grind down the cliff face
Rocks and pebbles smash against each other in the water, becoming rounded and smaller
Waves approaching the shore at an angle move sediment along the coast in a zigzag pattern
- Sediment is deposited when the energy of waves decrease, allowing the material to settle. This often happens in areas like bays and estuaries
- Headlands: high, rocky outcros of land that jut into the sea
- Bays: recessed coastal inlets, often with beaches, lying between headlands
- The sea erodes the softer rock lying perpendicular to the coast via processes like hydraulic action, abrasion and solution, forming bays
- The harder rock is more resistant and sticks out as headlands
- Over time, headlands become more exposed to erosion, while bays are more sheltered and often forming beaches
- Cliffs: steep, often vertical rock faces along the coast
- Wave-cut platforms: a flat area of rock in front of a cliff, exposed at low tide
1. Waves attack the base of a cliff through hydraulic action, abrasion and solution
2. This creates a wave-cut notch at the base of the cliff.
3. As the notch deepens, the cliff becomes unstable and eventually collapses.
4. The collapsed material is removed by the sea.
5. The cliff retreats inland, leaving behind a wave-cut platform.
6. This process continues, maintaining the steep profile of the cliff.
Headlands made of resistant rock
- Form when waves erode cracks or weaknesses in the headland.
- Hydraulic action and abrasion enlarge the crack into a cave.
- If the cave is eroded all the way through the headland, it becomes an arch
- The arch has a roof of rock and an open space beneath.
- The roof of the arch collapses due to gravity and continued erosion.
- This leaves an isolated pillar of rock called a stack
- The stack continues to be eroded at its base and may eventually collapse.
- The remains are known as a stump, often visible at low tide.
- Gently sloping landforms made of sand, pebbles, or shingle.
- Found between the high tide and low tide marks.
- Constructive waves build them up by depositing material.
- Can be sandy or shingle
1. Created by deposition of sediment from the sea.
2. Waves lose energy as they approach the shore, especially in sheltered bays.
3. Constructive waves with a strong swash and weak backwash carry material up the beach and deposit it.
4. Longshore drift moves material along the coast, shaping beaches and forming beach profiles.
- Hills of sand formed at the back of a beach
- Have a layered structure: from embryo dunes to grey dunes
- Often found in coastal areas with wide beaches and plenty of dry sand.
1. Dry sand is blown inland by the wind.
2. Sand accumulates around obstacles like driftwood or plants.
3. As more sand builds up, dunes form.
4. Marram grass helps stabilize dunes by trapping more sand with its roots and leaves.
5. Over time, dunes grow taller and move inland by succession
- Narrow strips of land made of sand or shingle.
- Project out into the sea from the coastline.
- Often curved at the end due to wave refraction or wind
1. Formed by longshore drift
2. When the coastline changes direction, the sediment is deposited.
3. Over time, this forms a spit.
4. If conditions remain calm, the spit extends further.
5. The end may curve due to wave action or prevailing wind direction.
- A bar is a ridge of sand or shingle that joins two headlands, blocking off a bay or lagoon.
- The water trapped behind the bar forms a lagoon.
1. A bar forms due to longshore drift
2. In cases where a bay has no strong river current, the spit can grow across it.
3. Eventually, it connects the two headlands, forming a bar.
4. Behind it, water is trapped and forms a lagoon
The Jurassic coast
1. Hydraulic action: is the force of moving water hitting the riverbanks and bed. Water enters cracks in the riverbank or bed, compresses air, and weakens the rock over time. Common in upper course where the flow is faster
2. Abrasion: Eroded material carried by the river scrapes and grinds against the bed and banks. It deepens and widens the river channel
3. Attrition: Rocks and stones in the river collide with each other. They break into smaller, rounder, and smoother pieces. Reduces sediment size as material moves downstream.
4. Solution: River water dissolves soluble rocks like limestone and chalk. It's a chemical process, not physical
1. Traction: Large boulders and rocks are rolled along the riverbed. The river doesn’t have enough energy to lift them, so it pushes them along the bottom. Common in the upper course of the river where the bed is steep.
2. Saltation: Small pebbles or stones are bounced along the riverbed in a leapfrogging motion. The river has enough energy to lift particles briefly, but not keep them suspended
3. Suspension: Fine, light materials like silt and clay are carried within the water itself. These tiny particles are suspended and flow with the current. Common in the lower course, where there’s more water. Gives rivers their muddy appearance.
4. Solution: Minerals are dissolved in the water and carried in solution. Water dissolves soluble rocks like limestone. Occurs throughout the river but especially in areas with soluble bedrock.
Interlocking spurs are ridges of land that jut into a river valley. They form in the upper course as the river winds around resistant rock due to vertical erosion.
1.A river flows over hard rock above soft rock.
2.The soft rock erodes quickly, forming a drop.
3. A plunge pool forms, undercutting the hard rock until it collapses.
4. This process repeats, and the waterfall retreats upstream.
A gorge is a steep-sided valley left behind as a waterfall retreats upstream through continued erosion and collapse of the overhanging rock
Meanders are bends in a river. They form when the river erodes the outer bank (forming a river cliff) and deposits on the inner bank (forming a slip-off slope), making the bend more pronounced over time.
An ox-bow lake is a U-shaped lake formed when a meander is cut off. The neck of the meander is breached during a flood, and deposition seals off the old loop.
Levées are raised riverbanks formed when a river floods. Heavy sediment is deposited closest to the river, building up natural embankments over time.
A floodplain is flat land beside a river. It forms through meander migration and sediment deposition during flooding, creating fertile land.
An estuary is the wide tidal mouth of a river where it meets the sea. It forms when river flow slows and deposits sediment, creating mudflats and salt marshes.