title: 'how does the channelcrossprofile and velocity on the riverholford change with distance downstream?'
justification of question: this question was chosen as we are studying theoretical channelcrossprofiles and what happens to velocity in rivers, so it is sensible to see if it is true in real life
we have to also consider where there is an interrelationship between the physical and human, we are therefore also going to ask: 'what is the impact on channel cross profile and velocity where humanintervention has taken place?'
aim: the purpose of the investigation is to determine how the channelcrossprofile and velocity of the velocity of the River Holford changes with distance downstream and if any of these changes are as a result of humanintervention
location: the source is in a wooded, steepvalley and stays steep for some time. its source is at lady'sfountain
location: the river then works its way into a flatterarea where flooding is a risk, for this reason, straighter drainagechannels have been built
location: the geology of the river consists of threedifferentrocktypes, at the source there is Devonian Quartzite - metamorphic, in the middle course there is Permo Marl - sedimentary and in the lower course - Jurassic Limestone - sedimentary
location: the first 2rocktypes are impermeable, which means that it is a fast reacting river to rainfallevents, but the third is permeable and so will lead to more infiltration lower down the river
feasibility: the investigation was carried out on the riverholford, at 10 different sites from source to mouth and the entire length is only 7.2kms long
feasibility: because the river is short, samples will be able to be taken along the length of the river over the course of the day
feasibility: the river is a suitable study area as the gradient generally decreases with distance downstream, whilst also having a variety of landuses and changes in the valleyshape, including geology
feasibility: it was only 1hour and 30minutes from school and is a publicright of way