Mountainous regions which have been shaped by glaciers
Glaciers are rivers of ice which once covered most of Britain
Processes of Erosion
1. Frost Shattering/freeze-thaw weathering
2. Plucking
3. Abrasion
Frost Shattering/Freeze-Thaw Weathering
Water freezes in cracks in rocks, expands and causes the rock to break into smaller pieces
Plucking
The water at the bottom of the glacier freezes onto rock on the valley base. As the glacier moves, the rock is pulled away from the valley base.
Abrasion
The rocks frozen into the glacier scour and scrape the valley sides and base, like sandpaper wearing away wood.
Corrie
Snow gathers in a hollow on the North facing side of a mountain
Ice moves downhill due to gravity
Plucking and abrasion deepen the hollow
After the ice melts, a large arm chair shaped corrie remains and water gathers in the bottom forming a tarn
Arête
Two corries form back to back
Plucking and frost shattering cause the back walls of the corries to retreat and steepen
The back walls have been eroded so far back that only a narrow ridge separates them
Frost Shattering has left the top of the ridge jagged
Pyramidal Peak
Three or more corries meet back to back
Abrasion and plucking deepen and steepen the back and base of the hollows
Narrow ridges called arêtes separate each corrie
The corries erode further back which creates a steep sided peak between them
Frost Shattering erodes the top of the mountain creating a pointed peak
Shaped Valley
Before the Ice Age, rivers in mountains ran in V shaped valleys
The glacier bulldozes through the valley, plucking and abrasion steepen the sides and deepen the floor
When the ice melts a U-shaped valley remains, sometimes with a misfit stream or ribbon loch
Truncated Spur
The spurs that used to interlock in the valley before glaciation have been removed by the bulldozing action of the glacier
Hanging Valley
Smaller tributary glaciers could not erode their valleys as deeply as the main glacier, so where they met, the tributary valley was left 'hanging' above the main valley
After glaciation these became waterfalls
Corries have a horseshoe shaped contour on maps, may have a corrie lake or tarn, and may be named as a 'corrie' or 'cwm' or 'Coire'
Arêtes have closely packed contour lines either side and often have rocky tops
Pyramidal peaks have a sharp summit and steep slopes on at least three sides, often seen as triangular on maps
shaped valleys have steep sides and a wide, flat floor, are usually straight and deep, with closely packed contours on the sides and few on the flat floor, may have a ribbon lake or misfit stream
Truncated spurs often have almost right angled contour lines, may have cliff symbols
Hanging valleys have contour lines 'wrapped round' the water and usually lead into U shaped valleys
National Park
An area of countryside designated for conservation and recreation, with restricted development
Land Use in Loch Lomond National Park
Forestry
Hill Sheep Farming
Tourism
Lots of tourists travelling to Loch Lomond
Leads to congestion on roads, increases noise and air pollution
Footpaths get bigger and bigger as walkers try to avoid muddy, worn parts
Creates a scar on the landscape and becomes an eyesore
People visiting Loch Lomond
Often leave their litter after a picnic or camping trip, creating an eyesore and danger for wildlife
Walkers leave gates open when walking through a field
Animals can escape, costing the farmer money and causing danger
Walkers take dogs off their lead while walking
Dogs have a natural instinct to chase sheep, which can be very dangerous and costly for the farmer
Wild camping and fires in the summertime
Create litter and increase the risk of accidents, especially in dry conditions when fires can spread
In 2017 the national park authority introduced byelaws restricting the right to camp along much of the shoreline of Loch Lomond, requiring permits for designated camping areas
Weather
The condition of the air at any one place at any given time
Elements of the Weather
Temperature
Precipitation
Wind
Humidity
Pressure
Weather instruments
Used to measure and record the weather
Found in weather stations on land, on ships, weather buoys, planes, weather balloons and satellites
Six's Thermometer
Measures the maximum and minimum air temperature, measured in degrees Celsius (°C)
Factors affecting the weather in the UK
Latitude
Distance from sea
Relief/Altitude
Aspect
Urban areas
Latitude
Describes how far a place is from the equator, temperatures generally decrease the further north you go
Distance from the sea
Water cools down more slowly than land, so the sea stays warmer for longer. In winter it is warmer in the West of the UK, in summer it is cooler in the West
Relief
Warm moist air rises over high land to the West of the UK, cooling and condensing to form clouds and rain. The dry air advances to the East.
Altitude
Upland areas are colder as temperatures decrease 1°C for every 100 metres gained in height. Wind speeds increase with altitude, affecting temperature.
Aspect
The direction in which land, a slope or a building faces, affecting how much sunshine a place receives and its temperature
Urban areas
Large towns and cities create heat from people, central heating and car use