How Well Does the River Tillingbourne Match the Bradshaw Model
- Submitted by: chiposaur
- Views: 142
- Category: Science
- Date Submitted: 11/11/2015 12:18 AM
- Pages: 14
- Report this Essay
How well does the River Tillingbourne match the Bradshaw Model?
As you travel further downstream a river, the rivers discharge increases. The water discharge increases as it flows downstream it meets more streams and also collects rain from the increased catchment area.
As you travel further downstream a river, the rivers discharge increases. The water discharge increases as it flows downstream it meets more streams and also collects rain from the increased catchment area.
Channel depth increases downstream. As there is an increased discharge, you have much more energy for erosion, also a larger body of water.
Channel depth increases downstream. As there is an increased discharge, you have much more energy for erosion, also a larger body of water.
The Bradshaw describes how a river's characteristics vary between the upper course and lower course of a river.
Load particle size decreases as you travel downstream. The load the river carries is broken down into smaller material via processes such as attrition.
Load particle size decreases as you travel downstream. The load the river carries is broken down into smaller material via processes such as attrition.
Although we haven’t studied the River Tillingbourne specifically, we have studied the River Severn, which has similar characteristics such as meanders. We should still expect similar features in aspects such as velocity and discharge. It is important to study rivers as it means you can research characteristics of a river, which can be used to gather data for things such as floods, which affect people’s lives drastically.
The River Tillingbourne
The river is located fairly near requiring a straightforward coach journey, meaning for convenience. It’s easily accessible (unlike Rivers such as the Thames, which is too deep and wide to measure) As well as it’s a fairly shallow river, making the means of collecting data much easier (As well as health and safety, so no chance of drowning). We were also...
As you travel further downstream a river, the rivers discharge increases. The water discharge increases as it flows downstream it meets more streams and also collects rain from the increased catchment area.
As you travel further downstream a river, the rivers discharge increases. The water discharge increases as it flows downstream it meets more streams and also collects rain from the increased catchment area.
Channel depth increases downstream. As there is an increased discharge, you have much more energy for erosion, also a larger body of water.
Channel depth increases downstream. As there is an increased discharge, you have much more energy for erosion, also a larger body of water.
The Bradshaw describes how a river's characteristics vary between the upper course and lower course of a river.
Load particle size decreases as you travel downstream. The load the river carries is broken down into smaller material via processes such as attrition.
Load particle size decreases as you travel downstream. The load the river carries is broken down into smaller material via processes such as attrition.
Although we haven’t studied the River Tillingbourne specifically, we have studied the River Severn, which has similar characteristics such as meanders. We should still expect similar features in aspects such as velocity and discharge. It is important to study rivers as it means you can research characteristics of a river, which can be used to gather data for things such as floods, which affect people’s lives drastically.
The River Tillingbourne
The river is located fairly near requiring a straightforward coach journey, meaning for convenience. It’s easily accessible (unlike Rivers such as the Thames, which is too deep and wide to measure) As well as it’s a fairly shallow river, making the means of collecting data much easier (As well as health and safety, so no chance of drowning). We were also...