Threats Facing Glaciated Landscapes (Edexcel A Level Geography)
Revision Note
Written by: Jacque Cartwright
Reviewed by: Bridgette Barrett
Threat of Natural Hazards
Active and relict glacial landscapes are inherently dangerous:
Avalanches
Rock falls
Debris slides
Flooding
Increased populations, developments, and tourism put people at risk within these areas
Avalanches
Avalanches are rapid movements of snow down a slope, and are common in mountainous areas
Avalanches occur when shear stress exceeds the shear strength of a mass of snow on a slope, which is linked to the snow's density and temperature
Two types of pack snow failure:
Loose snow - small amounts of snow move and roll down the slope
Slab avalanches - large 'slabs' of snow break away from underlying snow
This type of avalanche is the most dangerous
A large, fully-developed avalanche can weigh up to a million tonnes
Created when higher temperatures are followed by a freeze, creating an 'ice crust' on the surface, which is unstable
Avalanches start with a glide and then accelerate to speeds of 320km per hour (200m per hour), picking up even more snow as it rushes downhill
Occur most frequently on slopes over 22°
Also, occur on north-facing slopes where the lack of snow limits snow stability (doesn’t have time to bind with partial melting)
Three types of avalanches are:
New snow can fall off older snow (dry avalanche)
Or partially melted snow moves (wet avalanche)
Mostly from slab avalanches (powder avalanches)
A powder cloud forms with a large quantity of snow being suspended in the air
These are the most dangerous of avalanches
All avalanches are a significant hazard and kill approximately 200 people a year
Lahars
A lahar is a large mud and debris flow as a result of volcanic activity
Nevado del Ruiz, Colombia is known locally as the ‘sleeping lion’ and has not erupted for nearly 150 years
In the early hours of November 13th, 1985 it erupted
A combination of seismic activity, glacial instability, and extreme temperatures all combined to form one of the deadliest mudflows in history
Occurred during the night when most of the 27000 residents of Armero in Tolima were asleep
Armero was virtually destroyed by the 3-8m of mud and rubble that swept onto it and killed an estimated 23,000 people
Glacial outburst floods (GOFs)
Powerful floods caused by the sudden release of meltwater from a subglacial or ice moraine-dammed lake
Can be trigged in six ways:
Overflow and melting of the ice dam
Breakdown of ice dam due to tectonic activity
Increased rise in water levels
Mass movement creating an overtopping of the moraine dam through displacement
Catastrophic failure of moraine dam by slow ice melt within the moraine
Increased water pressure enlarging pre-existing tunnels beneath the ice dam
GOFs can be seasonal and dams can reform each year
These outbursts are sudden and pose a threat to property and people around the world
Meltwater can travel hundreds of kilometres from its sources and areas such as the Alps, Iceland, the Andes, and the Himalayas have a long history of GOFs
Periglacial areas are also seeing increased ground subsidence due to ice melt and flooding, risking new areas to sudden flooding
Threat of Human Activity
Glaciated landscapes face varying degrees of threat from human activities:
Urbanisation
Reservoir construction
Leisure and tourism
Urbanisation
Vary from isolated farms to nucleated towns depending on the location
Relict glaciated areas are traditionally agricultural with intermittent market towns
The impact varies on accessibility, but with the growth of tourism and the general population, many of these areas have seen a rise in development, pollution, and damage/loss of flora and fauna habitats
Infrastructure developments can damage permafrost and increase rates of melting through the release of greenhouse gases into the atmosphere
The exploitation of resources and discovery of new areas have increased risks of pollution by toxic waste from the mining of gold, copper, or uranium
Oil and gas spills into the polar waters have damaged the fragile balance of oceanic ecosystems which cascades onto land-based ecosystems
Reservoir construction
The construction of reservoirs in valleys is leading to landscape and hydrological changes
Upland glacial landscapes provide natural features for HEP and reservoir building
Power from HEPs provides power to urban areas
Reservoirs regulate water supplies
However, they also dramatically alter the landscape and impact a river's regime
The River Ganges rises in the Himalayas and discharges in Bangladesh
The glacial waters provide for many people, animals, and plants along its course
With the increased planned and constructed HEPs along its course, the impact is far-reaching with decreased water supplies and sediment supplies to areas downstream that rely on the river for their existence
Tourism
Places such as Antarctica have seen an increase in the number of tourists
Approximately 100,000 tourists visit Antarctica each year, and large cruise ships increase pollution in the area - both from the ship and the tourists themselves
Seeds from non-native species, caught on tourist clothing, are being seen growing in the ice-free coastal areas, threatening the continent's biodiversity
Adventure tourism to extreme cold environments is a growth industry for countries and local communities
Developments such as roads and hotels, disrupt wildlife and damage habitats and migratory patterns, leading to reduced biodiversity
In the European Alps, social mobility and wealth have increased the rate of deforestation for ski resorts and supporting infrastructure, leading to habitat loss and fragmentation
Tourism increases demand for energy and water resources
In Zemett, Switzerland, snow cannons add artificial snow to the slopes, but they are energy-intensive and add chemical and biological additives to the soil in the process
Relict glaciated landscapes are also under threat from tourism
Trekking causes damage to fragile mountain ecosystems
Plant communities, such as tundra flower meadows, need just 25 people a week and damage begins
Examiner Tips and Tricks
When discussing the impact of human activity across cold environments, do not just write about the impact on the landscape (e.g. deforestation for a new ski slope, or damage of permafrost for a new road etc.) You need to remember that the physical also includes a system approach of inputs, outputs, stores and flows (e.g. damage to permafrost from new road, releases carbon and methane to the atmosphere, increasing global warming and raising temperatures etc.) So human activity affects cold environments locally and globally but also the landscape features and the systems operating within on a short and long term basis.
Degradation of Landscape by Human Activity
Human activity can degrade the landscape and fragile ecology of glaciated landscapes through:
Soil erosion
Trampling
Landslides
Deforestation
Cold environments are fragile
Natural development and processes within cold environments occur slowly
They are long-term carbon and methane stores with a high albedo of up to 90% reflection of insolation
Any changes quickly cascade, and once damaged, it takes a long time for the ecosystem to recover, if at all
Adaptations of flora and fauna occurred over a long period of time, in order to survive their harsh surroundings
Plants and animals have to cope with a lack of daylight, climatic variations, and a very short growing season
Specialism, limited species numbers, sensitivity to changes, and slow development make this environment very fragile
Impacts
Ecosystems are resilient, however, they all have a threshold of tolerance and once crossed, can tip the ecosystem into a spiral of decline
Certain human activities have a bigger impact than others
Mountain biking or horse trekking are more damaging than walking
Deforestation and poor upland farming lead to soil erosion and landslides
Soil erosion is a major issue in the Andes, through over-cultivation and overgrazing on the slopes, in the need to provide subsistence for its growing populations
Exposed soils allow for weeds, resistant to erosion, to take over
Leisure activities damage ecosystems through trampling and compaction
Small leaves and delicate stems are damaged
This reduces photosynthesis, growth, and biomass
This provides less water and nutrients to the ecosystem
Continued trampling compacts the soil leading to poor soil condition, bare soil, and greater erosion
People will avoid rutted and exposed soil but fail to realise that walking on other areas leads to further damage
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