The characteristics of the Horsbere Brook vary along it length.

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The characteristics of the Horsbere Brook vary along it length.

Introduction

We followed the Horsbere Brook from its source in Buckholt Woods) to its confluence with the River Severn. We went to six places. They are Birdlip, Brockworth, Buckholt Woods, Innsworth, Hucclecote and Sandhurst. All these places are in the Cotswold Hills. The Cotswold Hills is made up of limestone, clay, chalk, sand and clays.

As I work through my coursework, I will try and answer the following questions below and I will also think about them as I go along my coursework.

  1. Does the depth of the River change from source to confluence?
  2. Does the width of the River change from source to confluence?
  3. Does the velocity of the River change from source to confluence?
  4. Does the bedload of the River become smaller in size from the source to confluence?

Picture of Meander: (Meander spotted at site    )

Meander - When rivers flow over a flatter land, they develop large bends called meanders. As a river goes around a bend most of the water is pushed towards the outside causing increased erosion.

Attrition - Material is moved along the bed of a river, it collides with other materials and breaks up into smaller pieces.

Corrasion – Fine material rubs against the river bank. The bank is worn away by a sand-papering action called abrasion and collapses.

 

Hydraulic action - The sheer force of the water hitting the banks of a river.

Traction – Large rocks and boulders are rolled along the bed of the river.

Saltation – Smaller stones are bounced along the bed of a river in a leap-frogging motion.

Suspension – Fine material, light enough in weight to be carried by the river, it is this material that discolours the water.

Solution – Dissolved material transported by the river.

Cross-section of a typical ridge and value landscape

Ridges and vales form a common landscape in many parts of south and east England. They occur in mainly resistant and permeable rocks alternate with mainly impermeable and less resistant rock. Softer limestone’s, such as chalk and Jurassic limestone, are porous. As water passes through them, they are resistant to erosion and so are left as rounded hills or as ridges where the rock has been tilted.

Spring – is pure water which is released from the ground e.g. the Horsbere Brook is a spring.

 

A river is a drainage basin which is an area of land which is drained by a river and its tributaries. We have seen the Horsbere Brook which is a tributary of the River Severn.

Data Interpretation

In the previous section which I worked on, which was data presentation where I drew graphs and pie-charts and now I will do an interpretation on the graphs  and I will also analyse my results.

At the first site we visited which was Birdlip, the environmental quality index was rated was rated high on the amount of vegetation, variety of vegetation, management of the area and the view but however the amount litter and buildings was given a low mark due to lots of litter being spotted at the site. Overall Birdlip was a beautiful place with an amazing view. Birdlip gained an over all mark of 27/35.

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View from Birdlip

We drew a pie chart of the land use at Birdlip. Half of the pie chart was taken up by the fields because majority of the site were fields. With the other half of the pie-cart, I split it into two for buildings and woods. There was a lot of natural scenery and vegetation at Birdlip. There was also a geological section at Birdlip.

Geological Section

At the second site we visited with was Buckholt Woods, the Environmental quality index was rated high due to the lack of buildings being present ...

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