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Geography Complete

Terms

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Freeze Thaw
breakup of rock by frost action. Must be plenty of precipitation, temperature must regularly rise above and fall below freezing pount. Occurs in mountainous areas and snow covered regions. Water seeps into the joints. Temp drops below zero and the water freezes and turns to ice and expands. Over time the repeated freeze thaw shatters the rock.
Waterfall
feature where water flows over a verticle slope. Hard or resistant rock lies on top of a band of soft rock. River erodes the soft rock more quickly than the hard rock.
Transportation
rivers are an agenty of transport. Traction, saltation, suspension, solution
Attrition
load itself worn down, smoothed and rounded.Process of erosion
Swallow hole
streams flow on lime stone surface, water widens the joints and stream dissaperes underground. Swallow hole is the shaft through which the rivver disappears.
Traction
larger particles (pebbels, stones) rolled allong the bed of the river.
Disadvantages of Tourism
Damage to flora/fauna. Change in quiet, unspoilt nature. Need to widen roads resulting in increased traffic & polution. Damage to monuments
Plungepool
feature of water fall. Falling watr cuts a hole called a plunge pool.
Active
Vesuvius (Italy)
Basalt
Igneous. Heavy, black. Lava cooled on the earths surface. Cooled to rapidly for any crystals to form. GIANT'S CAUSEWAY
Mid Atlantic Ridge
Deep under the atlantic ocean. fORMED BECAUSE THE NORTH AMERICAN PLATE IS PULLING AWAY FROM THE EURASIAN AND AFRICAN PLATE. Some are so high they reach above sea level to form volcanic islands (iceland)
The Burren
karst landscape in North Clare.
Anticlyne
Upward fold in a fold mountain.
Impermeable rock
ROCK THAT ISN'T ERRODED BY WATER
Pangaea
huge land mass that the continents of the world began as
Tributary
a small stream or river that joins up with a larger one
Marble
Metamorphic. White in colour but can chang depending on minerals present. Marble was formed from limestone. Hard rock, can be cut and polished. Found in CORK.
Seizmograph
measures the shockwaves of the earthquake
Delta
Triangular shaped area of land formed at the mouth of the river. River flows into the sea, loses its speed, deposits load of sediment. Tides & currents arent strong enough to carry it all out to the sea the deposits begin to build up. Mouth of the river soonb becomes clogged and the river brakes up in to smaller chanlles called distributaries.
Mechanical Weathering
Causes rock to be broken up into smaller pieces. Most likely to occur in areas of bare rock. E.g Freeze Thaw.
Upper or youthful stage
Valley has a narrow floor and steep sides. Steep gradient. Most of it's energy goes in to eroding.
Carbonation.
Occurs in Limestone landscapes. Rainwater takes in carbon dioxide as it passes through the atmosphere. Mixes with rain to form weak carbonic acid. Limestone contains calcium carbonate. Acid rain reacts with the calcium carbonate disolving it. Aided by weaknesses in limestone (joints).
Continental Drift
Plates float and move on the mantel.
Erosion
Breakdown of rocks and removal of the particles. cAUSED BY mOVING wATER, mOVIG ICE, MOVING AIR. Eventually deposited.
Open cast mining and quarrying
resource lies very close to the surface. Cheap but not friendly to the environmeant. Roadstone co. Peat - Bord na Mona.
Solution
dissolved load (limestone) is carried in a solution
Human activity
Cutting in to hillsides etc. Leaves slope steeper. Influences mass movement.
Sandstone
Seimentary. Coarse brown/red. Formed when large amounts of sand are worn from the earths crust, carried away and deposited on seabeds/lakes. The sand grains are slowly compressed and cemented to form rock. Macgillicuddy's Reeks.
Hekla
Volcanoe in Iceland
Focus
the place where an earthquake starts and shockwaves spread out from
Clints
blocks of limestone that speperate grikes
Syncline
Downward fold in a fold mountain
Landslides
rapid movement of regolith down a very steep slope. Landslides happen when the slope becomes unstable. (Quarrying, road building, erosion by sea. Heavy rain)
Acid Test
resr fir ckacuyn carbonate in soft rock like chalk/limestone. If it comes in contact with an acid (lemon juice) it fizzes.
Bog bursts
most common in upland area with peat. Large amounts of rainfall mean peat becomes saturated with water. Peat moves down slope quickly blocking roads and covering ffarmland.
Confluence
the point at which a tributary joins the river
Moh's Scale
Scale that grades the hardness of a mineral. Friedrich Mohs. Each mineral can be scratched by a mineral lower on the scale.
Course
the route a river takes as it flows into th esea
Transition Zone
Under the crust. Made of hot molten rock and other partly cooled semi solid rock substances.
Earth's Crust
the upper layer of the earthg averaging about 40km (25miles) thick. Solid Rock (Basalt, Granite)
Shaft Mining
resources lies in the seams deep beneath the surface. Verticel shafts to reach the seams. Extracts lead and zin ores. Navan, Lisheed. Galmoy.
Overhang
feature of waterfal. falling water cuts under the waterfall.
Curtain
continuous sheet of clacite formed when rainwater drips from a long crack in cavern roof
Levees
raised banks of alluvium. Floods begin to spread out over a flood plain, it looses its energy and begins to deposit its load. Heavier particles are deposited close to the river abnks. They build up to form levees. Missisippi.
Mouth
the point at which a river enters the sea or lake
Mudflows
very rapid mass movement. Occurs on both gentle and steep slopes. Occurs after torrential rain when soil is saturated and turns to mud.
Limestone Pavement
Large area of exposed limestone. Flat terraces, steep edges
Dormant
Cotopaxi (Peru)
Wider valley
sides of mature valley are less steep and the lfoor is wider and flat
Fold Mountains
Alps, Rockys, Andes.
Meanders
cirves or loops that develope along the course of a river. Formed by both erosion & deposition. River flows around a slighht ben the water on the outside band flows more quickly and has more power t erode. Water on the inner bank flows more slowly
Epicentre
The place on the surface area (directly above focus) where the earthquake hits the hardest
Alluvium
thin layer of very fertile clay on the flood plain
Armorican foldings
era when older fold mountains were formed. 250million years ago. Macgillicuddy's Reeks (Irish mountains)
Mass Movement
The movement of any loose material downslope under the influence of gravity.
Weathering
the breakdown and dec ay of rocks that are exposed to the weather (mechanical, chemical)
Plates
Parts that the crust is broken up in to
Hydraulic action
moving water breaks off material from the banks and bed of the river Process of erosion
Mid Ocean Ridge
long winding chain of mountains on the ocean floor that were formed by volcanic activity (plates seperating)
Cone shaped mountain volcanoes are made of
lava flow and ash layers
Karst Landscape
bare limestone landscape shows the effects of carbonation. THE BURRE
Passage
a long tunnel formed by underground streams
Innercore
Solid nickel. Solid due to immense pressure.
Extinct
Slemish (Antrim)
Watershed
high ground that seperates one basin from another
Convection Currents
currents of semi molten magma that plates move on
Alpine Foldings
era when young fold mountains were formed. 35 million years ago.
When plates colide..
Tremendous pressure. One plate sinks down in to the mantle and melts. Destructive boundarie. (Volcanic mountains, earthquakes, fold mountains)
Saltation
small sandsized particles are bounced along the bed of the river
Concave
outerbank
Basin
the land area from which a river and its tributaries drain water
Granite
Igneous. Hard, course, multicoloured. Feldspare and mica or quartz. Magma cooled deep within the earths crust. Cooled slowly to form large crystals.
Slate
Metamorphic. Formed from sedimentary rock shale.
Ox bow lakes
develope from well developed meanders. The neck of the land between the meanders becomes narrower. Flood cuts through it. Sediment deposited seals both ends. River now flows straight & ox bow lake is seperate
Middle or mature stage
Valley has a wider floor and the sides are more gently sloping. Gentle gradient. greater volume. Large load of material
Estuary
The part of the mouth that is tidal
Grikes
ejoints or cracks in the limestone that have been widened and deepend by weathering
Benefits of Tourism
increase in local employment . Spinoff benefits (pubs etc.) Reduction in outward migration. Improved services
Interlocking spurs
Areas of high ground that jut out and lock together. River meets obstacles and is unable to flow through them so it flows around them but contineues to erode downwards. Youthful landform
Richter Scale
scale of severity of the earthquake
Source
the lace where a river or stream begins
When plates push past one another..
Land is neither gained nor lost. Friction as plates push past eachother causes earth quakes.
Denudation
Solid and loose material of the earths crust being gradually worn down by a number of processes. Umbrella term.
Regolith
loose material like rock, soil and mud.
Limestone
Irelands most common rock. Sedimentary. Remains of fish and other sea creatures's skeletons pile up in shallow seas. Skeletons crushed by the weight of later deposits and cemented together by seawater. THE BURREN.
Scree
Sharp jagged pieces of rock broken off as a result of freeze thaw. Deposition/waste.
V-shaped valley
narrow floor and steep sides. Formed when a river cuts down into its bed by deepining it by vertical erosion & weathering breaks the sides. Youthful landform.
Soil Creep
Slowest type o fmass movement. Decreases with depth of the soil. Causes steps called terracettes in fields.
Fissure Eruption
A long crack in the earth's crust through which lava flows gently to the surface to spread out forming a plateau (example: Antrim Plateau)
Outercore
Molten due to very high temp.
Pacific Ring Of Fire
The worlds largest earthquake and volcanoe zone
When plates seperate..
Molten magma rises from the mantle where it cools to form a new crust. Constructive Boundary. (Volcanies, Mid-ocean ridges, islands)
lower or old age stage
Valley hasa sa wide, flat floor and gentle sides. Almost flat gradient. Large load. Mainly deposition.
Abrasion
the load of material carried along by the river hits the banks and bed of the river wearing them away Process of erosion
Water Content
The presence of water following heavy rain. Makes regolith heavier. Acts as lubricant
Gradient
The slope on which mass movement can occur. Influences Mass Movement
Chemical Weathering
Occurs when rocks decay or dissolve because of a chemical change. E.g CARBONATION.
solution
rocks disollved by the acids in the water. Process of erosion
Mantle
Magma. 4000 degrees celsious. Magma flows in slow moving currents
Quartzite
Variesin colours. Hard consists of quarts. Was fromed from sandstone. Forms pointed peaks on mountains. SUGARLOAF MOUNTAINS.
Floodplain
level area of land on either side fo the river. has a covering of alluvium. alluvium is built up over many periods of flooding.
Offshore Drilling
takes place where oil and gas are found under the sea bed. Rig/pipeline. Kinsale Head. Corrib gas field.
Convex
inner bank
Suspension
lightest particles (silt) are carried along suspended in the water

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