Compare the observations and recordings made at the two sites with predictions made from the characteristics of a 'theoretical' river.
- Words:
- 3636
- Submitted:
- Tue Aug 05 2003

Have a little read: ... Introduction At the beginning of July 2002, we went to study two sites on the River Bovey in Devon. The initial site of enquiry was at the source of the river (Site 1 - grid reference SX 694829) where we collected data on the characteristics of the bedload, the velocity of the water and the cross-sectional area and bankfull level of the river. We then repeated this data collection at a second location (Site 2 - SX 779801) approximately 15km downstream near the mid-point of the river's course. The River Bovey is situated inside the Dartmoor National Park in the Southwest of England. Dartmoor is a large intrusive granite landform with many areas exposed through years of erosion and weathering. The moorland's high altitude results in extensive amounts of relief rainfall which, along with the park's impermeable rock-type, means the area has a high drainage density. These factors also mean that the
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