Mapa mental
Carlisle Floods 2005
Contenido del mapa
Carlisle Floods 2005
Impacts
- Affected 2,700 homes
- 3 people died
- Cost of damage estimated to be £400 million
- Flooded services such as fire stations and police stations
Causes of flooding
- Vegetation
- Mixed arable and grassland in valleys and rough hill pasture on uplands
- Due to the floods taking place in January, there is less vegetation, decreasing interception making peak discharge higher. Farmland means more compacting soil reducing infiltration
- Mixed arable and grassland in valleys and rough hill pasture on uplands
- Geology
- Includes impermeable slate and volcanic rocks in Skiddaw area and sandstone and limestone in the Vale of Eden
- Due to Carlisle lying on impermeable rock, the water is not absorbed into the soil properly, meaning the water reaches the river more quickly
- Includes impermeable slate and volcanic rocks in Skiddaw area and sandstone and limestone in the Vale of Eden
- Soils
- Thin soils on much of the upland area, deeper soils and alluvium in the valleys
- Thin soils means difficult infiltration as they can't cope with the water volume
- Thin soils on much of the upland area, deeper soils and alluvium in the valleys
- Rainfall
- Intense rainfall 201,286,000m^3 leading to a 73% runoff of 147,205,000m^3
- Heavy rainfall on soil which is saturated from a previous period creates over flooding. The intensity and duration also effects this as the infiltration capacity of the soil is exceeded
- Intense rainfall 201,286,000m^3 leading to a 73% runoff of 147,205,000m^3
- Relief
- Significant areas of upland with steep slopes characterise much of the upper basin. Much lower gradients around Carlisle
- Water will not infiltrate if on a steep slope as all of the water will want to go down the hill
- Significant areas of upland with steep slopes characterise much of the upper basin. Much lower gradients around Carlisle
- Urbanisation
- Limited in upland regions, increasing spread of towns and villages in valley areas
- There is an increase on the rate o impermeable rock which decreases the amounts of soil. Water is drained and pumped back into the river
- Limited in upland regions, increasing spread of towns and villages in valley areas
- Basin shape and size
- The rivers Caldew, Petteril and Birthing have a confluence with the Eden just before or in Carlisle itself
- Carlisle is built on a confluence meaning there is water from two river
- The rivers Caldew, Petteril and Birthing have a confluence with the Eden just before or in Carlisle itself
- Vegetation
Key Facts
- Carlisle is situated on the floodplain of the River Eden with three river meeting in the city
- Eden
- Petteril
- Irthing
- The catchment is mainly rural which covers 2,400km^2
- It is home to 244,000 people
- Carlisle is situated on the floodplain of the River Eden with three river meeting in the city
Información
- Descripción
- AS - Level (Rivers) Geography Mapa Mental sobre Carlisle Floods 2005, creado por Joanne Spain el 23/03/2016.
- Creado por
- Joanne Spain
- Visitas
- 6
- Valoración