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Adder Bottom

Valley in Sussex Mid Sussex

England

Adder Bottom

Devil's Dyke View Point Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk <span class="nowrap"><a title="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex" rel="nofollow ugc noopener" href="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
Devil's Dyke View Point Credit: PAUL FARMER

Adder Bottom is a picturesque valley located in the county of Sussex, England. Nestled in the South Downs National Park, it is renowned for its natural beauty and tranquil surroundings. The valley is characterized by rolling hills, verdant meadows, and a meandering river that flows through its heart.

The name "Adder Bottom" is derived from the presence of adders, a type of venomous snake, which historically inhabited the area. However, due to conservation efforts, the population of adders has significantly decreased in recent years, making sightings rare.

The valley is home to a diverse range of flora and fauna. Wildflowers such as bluebells and primroses carpet the meadows in spring, attracting a variety of butterflies and bees. The river and its banks provide a habitat for numerous species, including otters, kingfishers, and herons.

Hikers and nature enthusiasts are drawn to Adder Bottom for its extensive network of walking trails. The area offers breathtaking views from the hilltops, making it a popular destination for photographers and artists. Additionally, the valley is a haven for birdwatchers, as it attracts a wide variety of bird species throughout the year.

Despite its natural beauty, Adder Bottom remains relatively untouched by human development. There are no towns or villages within the valley itself, creating an unspoiled and peaceful environment. Visitors can experience a sense of tranquility as they explore the valley and immerse themselves in its enchanting atmosphere.

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Adder Bottom Images

Images are sourced within 2km of 50.875945/-0.21828887 or Grid Reference TQ2510. Thanks to Geograph Open Source API. All images are credited.

Devil's Dyke View Point Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk <span class="nowrap"><a title="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex" rel="nofollow ugc noopener" href="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
Devil's Dyke View Point
Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk LinkExternal link
Ferns near the bottom of Devil's Dyke
Ferns near the bottom of Devil's Dyke
Devils Dyke from North Hill One of the most spectacular dry valleys in the South Downs.
Devils Dyke from North Hill
One of the most spectacular dry valleys in the South Downs.
Fulking - from the South Downs This is a cross-grid shot. The camera was in the square to the south.
Fulking - from the South Downs
This is a cross-grid shot. The camera was in the square to the south.
Tree and reflection A collection of photographs taken around midday by Geographers from all over Britain and Ireland. See all the images on the map: <a title="https://www.geograph.org.uk/stuff/xmas.php?year=2022" href="https://www.geograph.org.uk/stuff/xmas.php?year=2022">Link</a>
Tree and reflection
A collection of photographs taken around midday by Geographers from all over Britain and Ireland. See all the images on the map: Link
Inscription by the spring
Inscription by the spring
Devil's Dyke The day after Boxing Day 2022, one which began wet and gloomily before brightening before clouding over and getting quite chilly.
Devil's Dyke
The day after Boxing Day 2022, one which began wet and gloomily before brightening before clouding over and getting quite chilly.
Viewpoint at Devil's Dyke Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk <span class="nowrap"><a title="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex" rel="nofollow ugc noopener" href="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
Viewpoint at Devil's Dyke
Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk LinkExternal link
Devil's Dyke Country Pub & Dining
Devil's Dyke Country Pub & Dining
Trig point at Devil's Dyke Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk <span class="nowrap"><a title="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex" rel="nofollow ugc noopener" href="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
Trig point at Devil's Dyke
Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk LinkExternal link
View through a window A derelict building at Devil's Dyke, with a view through the window towards Fulking.
View through a window
A derelict building at Devil's Dyke, with a view through the window towards Fulking.
View from Devil's Dyke across the Low Weald
View from Devil's Dyke across the Low Weald
The South Downs near Fulking The South Downs is one of the four areas of chalk downland in southern England. They extend from the eastern side of Hampshire through Sussex, culminating in the cliffs at Beachy Head. The South Downs is England's newest National Park, its designation taking effect on March 31, 2010. There are many Sites of Special Scientific Interest within the park. The area is relatively unpopulated, although along its southern periphery there is an almost uninterrupted ribbon of seaside towns. It is extremely popular with walkers, having one principal long distance footpath, the South Downs Way, and many interconnecting ones. There are three principal gaps in the upland through which rivers flow; and there are also many dry valleys along its length. The South Downs have a long history; there are archaeological remains from Neolithic times. Until the middle of the 20th century, sheep-rearing was the main occupation of those living on the Downs. At 886ft, Butser Hill is the highest point of the South Downs. Extract from Wikipedia <span class="nowrap"><a title="http://en.wikipedia.org/wiki/South_Downs" rel="nofollow ugc noopener" href="http://en.wikipedia.org/wiki/South_Downs">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
The South Downs near Fulking
The South Downs is one of the four areas of chalk downland in southern England. They extend from the eastern side of Hampshire through Sussex, culminating in the cliffs at Beachy Head. The South Downs is England's newest National Park, its designation taking effect on March 31, 2010. There are many Sites of Special Scientific Interest within the park. The area is relatively unpopulated, although along its southern periphery there is an almost uninterrupted ribbon of seaside towns. It is extremely popular with walkers, having one principal long distance footpath, the South Downs Way, and many interconnecting ones. There are three principal gaps in the upland through which rivers flow; and there are also many dry valleys along its length. The South Downs have a long history; there are archaeological remains from Neolithic times. Until the middle of the 20th century, sheep-rearing was the main occupation of those living on the Downs. At 886ft, Butser Hill is the highest point of the South Downs. Extract from Wikipedia LinkExternal link
Inside a derelict building at Devil's Dyke
Inside a derelict building at Devil's Dyke
Woodland and path at Devil's Dyke Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk <span class="nowrap"><a title="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex" rel="nofollow ugc noopener" href="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
Woodland and path at Devil's Dyke
Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk LinkExternal link
Devil's Dyke Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk <span class="nowrap"><a title="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex" rel="nofollow ugc noopener" href="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
Devil's Dyke
Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk LinkExternal link
Road at Devil's Dyke Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk <span class="nowrap"><a title="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex" rel="nofollow ugc noopener" href="http://en.wikipedia.org/wiki/Devil%27s_Dyke,_Sussex">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span>
Road at Devil's Dyke
Devil's Dyke is a V-shaped valley on the South Downs Way in southern England, near Brighton and Hove. It is part of the Southern England Chalk Formation. The 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk LinkExternal link
Road near Devil's Dyke
Road near Devil's Dyke
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Adder Bottom is located at Grid Ref: TQ2510 (Lat: 50.875945, Lng: -0.21828887)

Administrative County: West Sussex

District: Mid Sussex

Police Authority: Sussex

What 3 Words

///tables.blackmail.memory. Near Portslade, East Sussex

Nearby Locations

Devil's Dyke Fulking Hill Adder Bottom

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The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.
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