1/44
Name | Mastery | Learn | Test | Matching | Spaced |
---|
No study sessions yet.
Open Systems
Systems where energy and matter can enter and leave through inputs and outputs.
Closed Systems
Systems where matter cannot enter or leave; only energy can enter and leave.
Dynamic Equilibrium
A state where there is a balance between inputs and outputs in a system.
Positive Feedback
Processes that lead to an increase or growth, moving away from dynamic equilibrium.
Negative Feedback
Processes that lead to a decrease or decline, restoring balance in a system.
Littoral Zone
The area of the shoreline affected by wave action, divided into subzones.
Backshore
The part of the beach lying between the beach face and the vegetation line, usually dry.
Foreshore
The area between the high and low tide marks.
Inshore
The area between the low water mark and where waves cease to influence the land.
Offshore
The area of deeper water beyond the breaking waves.
Nearshore
Shallow water beyond low tide where wave interaction occurs.
Swash Zone
The upper part of the beach between backbeach and the surf zone, subject to intense erosion.
Surf Zone
The nearshore area where waves come onto the beach.
Breaker Zone
The offshore area where waves break, typically in depths of 5m-10m.
Fetch
The distance of open water over which the wind blows.
Wave Refraction
The distortion of wave fronts as they approach a shore, causing varying energy levels.
Longshore Drift
The movement of sediment along the beach due to wave action.
Rip Currents
Strong underwater currents moving away from the shoreline.
Upwelling
The movement of cold, nutrient-rich water from the deep ocean to the surface.
Tides
Changes in sea level caused by the gravitational pull of the moon and sun.
Tidal Range
The difference in height between high and low tides.
Hydraulic Action
The impact of water force on coastal rocks, leading to erosion.
Wave Quarrying
The process where air trapped in wave action causes rock fragments to break off cliffs.
Attrition
The process where rocks collide with each other, wearing down over time.
Abrasion
The rubbing of sediment against rocks, causing erosion.
Solution (Erosion)
The dissolving of rocks in water.
Lithology
Study of the physical and chemical characteristics of rocks.
Clastic Rocks
Rocks composed of sediment particles that are cemented together.
Crystalline Rocks
Rocks made of interlocking mineral crystals.
Unconsolidated Sediment
Sediment that has not been cemented to form solid rock.
Rock Class
Categories of rock such as sedimentary, igneous, or metamorphic.
Strata
Layers of rock that reflect periods of geological time.
Bedding Plane
Horizontal natural breaks in sedimentary rock layers.
Joints
Vertical fractures in rocks caused by contraction or stress.
Folds
Bends in rock layers caused by tectonic forces.
Faults
Fractures in Earth's crust where rocks have moved.
Traction
Transport of large stones and boulders rolled along the sea bed.
Saltation
Bouncing movement of small stones and pebbles along the sea bed.
Suspension
Transport of fine particles suspended in water by wave action.
Deposition
When sediment accumulates faster than it is removed.
Physical Weathering
Breakdown of rocks through mechanical processes without chemical change.
Chemical Weathering
Alteration of rock through chemical reactions, such as dissolution.
Hydrolysis
Chemical process where water reacts with minerals to create new materials.
Mass Movement
The movement of rock and soil down slopes, influenced by gravity.
Cohesion
The degree to which materials stick together, affecting mass movement.