Summer Down

Downs, Moorland in Sussex Mid Sussex

England

Summer Down

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

Summer Down is a picturesque area located in the county of Sussex, England. It is characterized by its rolling hills, expansive grasslands, and diverse flora and fauna. Situated in the South Downs National Park, Summer Down offers breathtaking views and an abundance of outdoor activities for nature enthusiasts.

The landscape of Summer Down is dominated by the iconic chalk hills of the South Downs, which provide a stunning backdrop to the area. These hills are interspersed with deep valleys and steep slopes, creating a varied and dynamic terrain. The area is also home to several large open spaces, including meadows and heathlands, which are teeming with wildflowers during the summer months.

The flora and fauna of Summer Down are incredibly diverse. The grasslands are adorned with vibrant wildflowers such as harebells, ox-eye daisies, and orchids, attracting a wide variety of butterflies and bees. The heathlands are home to rare species like the silver-studded blue butterfly and the Dartford warbler. The area also supports a healthy population of mammals, including deer, foxes, and badgers.

Outdoor activities in Summer Down are plentiful, making it a popular destination for hikers, cyclists, and nature lovers. The South Downs Way, a long-distance footpath, passes through the area, offering breathtaking views of the surrounding countryside. Additionally, there are numerous trails and bridleways that wind through the hills, providing opportunities for exploration and adventure.

In conclusion, Summer Down is a captivating area in Sussex, boasting stunning landscapes, diverse flora and fauna, and a plethora of outdoor activities. It is a haven for nature enthusiasts seeking a peaceful retreat or an adrenaline-filled adventure amidst the beauty of the South Downs.

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Summer Down Images

Images are sourced within 2km of 50.885521/-0.19882985 or Grid Reference TQ2611. 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
Forge Garage - old filling-station paraphernalia
Forge Garage - old filling-station paraphernalia
Saddlescombe from North Hill Much of the land here is owned and managed by the National Trust.
Saddlescombe from North Hill
Much of the land here is owned and managed by the National Trust.
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.
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.
Winter trees on Newtimber Hill
Winter trees on Newtimber Hill
View west over Poynings from North Hill Chanctonbury Ring can be seen in the distance.
View west over Poynings from North Hill
Chanctonbury Ring can be seen in the distance.
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
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Summer Down is located at Grid Ref: TQ2611 (Lat: 50.885521, Lng: -0.19882985)

Administrative County: West Sussex

District: Mid Sussex

Police Authority: Sussex

What 3 Words

///touches.respond.unlocking. Near Portslade, East Sussex

Related Wikis

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Nearby Amenities

Located within 500m of 50.885521,-0.19882985
Barrier: stile
Lat/Long: 50.8891444/-0.2013001
Bicycle: no
Foot: yes
Horse: no
Motor Vehicle: no
Lat/Long: 50.886793/-0.2055272
Crossing
Lat/Long: 50.8860529/-0.1943251
The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.

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