River Holford Background and Theory
- Created by: zelahl32
- Created on: 17-11-16 08:31
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- Location
- Quantock Hills, Somerset
- Geography Unit 2 - River Holford Background and Theory
- Land use
- Upper course
- Heavily wooded area
- Steep slopes
- Impermeable Devonian Quartzite
- Middle course
- Lower course
- Low gradient, shrubs (bilberry), bracken, grasses
- Upper course
- Land use
- 7.5km long
- Source of river
- Lady's Fountain Springs, Robin Upright's Hill
- 250m above sea level
- Lady's Fountain Springs, Robin Upright's Hill
- Mouth of river
- At Kilve meeting Bridgewater Bay
- Geology of the area
- Devonian Quartzite (Metamorphic) upper course
- Location
- Quantock Hills, Somerset
- Geography Unit 2 - River Holford Background and Theory
- Land use
- Upper course
- Heavily wooded area
- Steep slopes
- Impermeable Devonian Quartzite
- Middle course
- Lower course
- Low gradient, shrubs (bilberry), bracken, grasses
- Upper course
- Land use
- 7.5km long
- Source of river
- Lady's Fountain Springs, Robin Upright's Hill
- 250m above sea level
- Lady's Fountain Springs, Robin Upright's Hill
- Mouth of river
- At Kilve meeting Bridgewater Bay
- Permo-Triassic Marl (Sedimentary) middle course
- Jurassic Limestone (Sedimentary) Lower course
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