Physical Geography Ez Flashcards
The Earth’s Layers
Crust
● Mantle
● Outer core
● Inner core
Plates
● 7 major plates
● Destructive plates (two colliding plates)
● Constructive plates (two separating plates)
Convectional currents
The very hot core heats the magma
● Convectional currents are set up in the mantle
● Molten magma moves upwards from the core towards the crust
● At the crust, the magma cools and sinks back down towards the core so the cycle can
start over again
● There is friction between the convectional currents and the plates
● The friction causes the plates to move slowly on top of the mantle
● As a result, the plates may collide or pull apart from each other
Mid-ocean ridge
Underwater mountain range
● Formed where two plates separate
● As the plates move apart, molten magma rises from the mantle and fills the gap between
the plates
● When the magma meets the cold seawater, it cools and solidifies to form a new ocean
floor
● As the eruptions of magma continue in an endless cycle, the ocean floor is built up to
form a long ridge of mountains
Volcanoes
Magma from the magma reservoir reaches the surface through a v ent which may erupt
violently, blasting materials into the sky through the crater
● When magma reaches the surface, it’s known as lava
● Lava pours out of the crater and flows down the side of the cone, cooling and hardening
● Other materials may also come out during the eruption
● Layers of these materials build up to form a cone shaped mountain
Types of volcanoes
● Active volcanoes still erupt on a regular basis e.g Mount Vesuvius
● Dormant volcanoes erupted in the past but may not erupt again e.g Mount Cotopaxi
● Extinct volcanoes have not erupted in historic times e.g Mount Slemish
Advantages of volcanoes
Fertile soil
● Precious stones and minerals can be originated in volcanoes
● Building materials from rocks formed as a result of volcanic eruption (igneous rocks)
● Hot springs and geysers can be used to generate electricity
● Volcanoes attract tourists
Disadvantages of volcanoes
Loss of life
● Damage to property
● Destroys wildlife and the environment
Pacific Ring of Fire
Active volcanoes that surround the Pacific Ocean
Fold mountains
They are found along plate boundaries
● When two plates collide, the rocks tend to buckle and crumple upwards into a series of
folds
● Large amounts of compression occurs
● Armorican fold mountains are smaller in size because they are older and have been
severely worn done
● Alpine fold mountains are larger in size because they are younger and have not been as
severely worn down
Earthquakes
● An earthquake is a sudden movement or trembling or the Earth’s crust
● This movement takes the form of a series of shocks or tremors
● Earthquakes occur at boundaries where plates collide
● As the plates push into one another pressure builds up until one of the plates slips
● The plates move along the f ault lines
● The focus is the point deep in the Earth’s crust where the earthquake begins
● The tremors spread out from the focus
● The epicentre is the point on the surface directly above the focus and this is the place
where tremors are the strongest
Effects of Earthquakes
Builds collapse, especially those that are closer to the epicentre
● Roads begin to crack and railway lines start to bend
● Fires may occur when gas pipes break
● Tsunamis can result from underwater earthquakes
Reducing Impact of Earthquakes
Build buildings that sway with minor earthquakes
● Scientists should examine seismographs to predict potential earthquakes
Richter Scale
Measures and determines the strength of earthquakes
Basalt is an igneous rock
● Formed when lava cools down from volcanic activity over a short period of time
● It cools very quickly and usually within a few hours
● It’s formed when the lava spreads out across the Earth’s surface
● The lava quickly solidifies when it is exposed to air
● Basalt has tiny crystals that can’t be seen by the naked eye
● Basalt can be found at the Giant’s Causeway in Co. Antrim
Granite is an igneous rock
● Formed when molten magma cools down from volcanic activity over a long period of
time
● Molten magma forces its way into the crust
● It cools very slowly in the Earth’s crust over millions of years allowing large crystals to
form
● The crystals formed include quartz and mica
● Granite eventually comes to the surface when the overlying rocks wear away
● Granite can be found in Mourne and the Wicklow Mountains
Limestone and sandstone are sedimentary rocks
Limestone
● Formed on the beds of shallow, warm seas from the skeletons of tiny sea creatures, fish
and shells
● These skeletons piled up over millions of years
● They were compressed and cemented together because of the water pressure
● Some fossils are still preserved on the rocks
● The color of limestone ranges from white to grey
● They are permeable (water can easily pass through) and laid in strata (horizontal layers
known as bedding planes)
● Limestone can be found in 31 out of the 32 counties in Ireland
● Limestone is eroded easily by carbonation because calcium carbonate (limestone)
reacts with acidic rainwater
● Uses of limestone: M anufacturers use limestone for cement
Builders use limestone to make public buildings and road surfaces Farmers use ground up limestone as soil conditioner
2. Sandstone
● Formed when large amounts of sand were worn away from the Earth’s surface and transported by the wind and rivers
● The sand was deposited on seabeds and deserts
● Layers built up, compressed and cemented to eventually form sandstone
● Sandstone varies in color from brown to red
● Sandstone can be found in the Magillicuddy Reeks and the Galtees
Marble and quartzite are metamorphic rocks
Marble
● Formed when magma forces its way into limestone which puts the limestone under great pressure and heat
● Great pressure and heats changes limestone into the rock marble
● Pure marble is white
● Marble is a hard rock and contains crystals
● Easily polished and cut
● In demand for furniture and ornaments
● Found on Rathlin Island and in Connemara
2. Quartzite
● Formed when sandstone was put under great pressure and heat in the Earth’s crust
● Usually forms during periods of folding
● Contains mainly grains of quartz packed tightly together
● Varies from grey to white
● Extremely hard rock
● Found in Croagh Patrick and Errigal
Drilling
Extracts oil or gas from an underground reservoir
● Most takes place on land
● If offshore, a pipeline on the seabed brings the fuel up