Newtimber and Pangdean

Heritage Site in Sussex Mid Sussex

England

Newtimber and Pangdean

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

Newtimber and Pangdean, located in Sussex, England, are two neighboring areas that hold significant historical and cultural value. Both sites are renowned for their rich heritage and offer visitors a glimpse into the past.

Newtimber is a small village nestled within the South Downs National Park. It is most notable for its picturesque 11th-century church, St. John the Evangelist. This Norman church is a prime example of medieval architecture, with its sturdy flint walls and a beautiful wooden spire. The interior features an intricately carved Norman font, ancient stained glass windows, and a collection of historical artifacts. The churchyard itself is a peaceful haven, dotted with ancient gravestones and offering stunning views of the surrounding countryside.

A short distance away lies Pangdean, a historic farmstead that dates back to the 16th century. The farm is known for its charming traditional buildings, including a timber-framed farmhouse and a historic barn. These structures provide a unique insight into the rural life of Sussex's past. Pangdean has been lovingly preserved and is still a working farm, with fields grazed by cattle and sheep.

Both Newtimber and Pangdean offer visitors the opportunity to connect with the area's rich history and natural beauty. The sites are often visited by history enthusiasts, photographers, and those seeking a peaceful retreat in the countryside. The surrounding landscapes of rolling hills, lush meadows, and quaint villages further add to the charm and allure of these heritage sites. Whether exploring the ancient church or strolling through the idyllic farmstead, visitors to Newtimber and Pangdean are sure to be captivated by their timeless appeal.

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Newtimber and Pangdean Images

Images are sourced within 2km of 50.894/-0.196 or Grid Reference TQ2612. 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
View WSW along the South Downs from Wolstonbury Hill
View WSW along the South Downs from Wolstonbury Hill
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
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Newtimber and Pangdean is located at Grid Ref: TQ2612 (Lat: 50.894, Lng: -0.196)

Administrative County: West Sussex

District: Mid Sussex

Police Authority: Sussex

What 3 Words

///roof.wiggles.shrubbery. Near Hassocks, West Sussex

Related Wikis

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Saddlescombe Preceptory

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Newtimber

Newtimber is a small village and civil parish in the Mid Sussex District of West Sussex, England. It is located north-west of Brighton. The parish also...

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Beeding Hill to Newtimber Hill

Beeding Hill to Newtimber Hill is a 321 ha (790-acre) biological and geological Downland Site of Special Scientific Interest (SSSI) north of Shoreham-by...

Wolstonbury Hill

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Nearby Amenities

Located within 500m of 50.894,-0.196
Newtimber Hill
Created By: Potlatch 0.10f
Natural: peak
Source: NPE
Lat/Long: 50.8981407/-0.1949124
Description: Uninterrupted and far reaching viewpoint across; Lower Weald, Downland and Sea
Direction: 270
Tourism: viewpoint
Lat/Long: 50.8964235/-0.1945106
Barrier: stile
Lat/Long: 50.890725/-0.1998433
Barrier: stile
Lat/Long: 50.8925234/-0.2001557
The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.

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