Appletreewick

Civil Parish in Yorkshire Craven

England

Appletreewick

B6265 on Fancarl Top Approaching the turning for Appletreewick
B6265 on Fancarl Top Credit: David Smith

Appletreewick is a charming civil parish located in the Craven district of North Yorkshire, England. Situated in the picturesque Yorkshire Dales National Park, this small village is surrounded by stunning natural beauty and offers a tranquil escape from the bustling city life.

The village is nestled in the valley of the River Wharfe, with rolling hills and lush greenery providing a breathtaking backdrop to the area. Appletreewick is known for its idyllic countryside views, with many walking trails and hiking routes attracting outdoor enthusiasts and nature lovers.

The village itself is home to a close-knit community, with a population of around 140 people. The traditional stone-built houses and charming cottages give Appletreewick a timeless appeal, while the local pub, the Craven Arms, is a popular gathering spot for both locals and visitors.

One of the village's main attractions is the stunning natural landmark, Parcevall Hall Gardens. These beautiful gardens are known for their extensive collection of plants and flowers, offering visitors a peaceful retreat to explore and enjoy.

Appletreewick is also famous for its annual scarecrow festival, where creative and imaginative scarecrows are displayed throughout the village, delighting both children and adults alike.

With its rich history, natural beauty, and friendly community, Appletreewick is a hidden gem in the heart of Yorkshire. Whether you're looking to escape the hustle and bustle of city life or explore the great outdoors, this quaint village has something to offer everyone.

If you have any feedback on the listing, please let us know in the comments section below.

Appletreewick Images

Images are sourced within 2km of 54.069542/-1.892923 or Grid Reference SE0763. Thanks to Geograph Open Source API. All images are credited.

B6265 on Fancarl Top Approaching the turning for Appletreewick
B6265 on Fancarl Top
Approaching the turning for Appletreewick
B6265 east of Dibble's Bridge The road descends to cross the River Dibb before approaching Hebden.
B6265 east of Dibble's Bridge
The road descends to cross the River Dibb before approaching Hebden.
Straight across the moor The drystone walls at Jack Hole Flat run in straight lines and are an indication of 19th century parliamentary enclosures. In the distance can be seen the gritstone outcrop of Wig Stones.
Straight across the moor
The drystone walls at Jack Hole Flat run in straight lines and are an indication of 19th century parliamentary enclosures. In the distance can be seen the gritstone outcrop of Wig Stones.
Gritstone and Limestone Life gets complicated geology-wise around here. An outcrop of carboniferous limestone to the right is only a few metres from a couple of large gritstone boulders which look to be on the surface as opposed to part of the strata. Maybe they were dumped here by a glacier.
Gritstone and Limestone
Life gets complicated geology-wise around here. An outcrop of carboniferous limestone to the right is only a few metres from a couple of large gritstone boulders which look to be on the surface as opposed to part of the strata. Maybe they were dumped here by a glacier.
Limestone outcrop, Nursery Knot A view from the summit area of Nursery Knot across moorland towards Grimwith Reservoir. On the horizon can be seen the hump of Great Whernside with a thin cover of snow.
Limestone outcrop, Nursery Knot
A view from the summit area of Nursery Knot across moorland towards Grimwith Reservoir. On the horizon can be seen the hump of Great Whernside with a thin cover of snow.
Summit rocks, Nursery Knot This small hill to the north of the B6265 has a summit crowned by an outcrop of carboniferous limestone which dips quite steeply to the north. The rocks of the Yorkshire Dales are stacked one on top of the other in almost level layers - with a gentle dip towards the north east, but here everything changes as this site is close to the Craven fault zone where rock has been put under great pressure and pushed out of shape. The limestone here is part of a thin finger which stretches eastwards for another 2 or 3 miles to Coldstones Quarry before fading out above Pateley Bridge.
Summit rocks, Nursery Knot
This small hill to the north of the B6265 has a summit crowned by an outcrop of carboniferous limestone which dips quite steeply to the north. The rocks of the Yorkshire Dales are stacked one on top of the other in almost level layers - with a gentle dip towards the north east, but here everything changes as this site is close to the Craven fault zone where rock has been put under great pressure and pushed out of shape. The limestone here is part of a thin finger which stretches eastwards for another 2 or 3 miles to Coldstones Quarry before fading out above Pateley Bridge.
Pockmarked hillside near Stump Cross Looking almost like shell holes from an old battlefield, these dips and hollows are almost certainly the work of man. Note also the line of hollows running across the photo higher up. All these features are due to lead workings, the higher line following a vein across the moor. This area close to the B6265 is also close to the eastern end of the Craven fault zone, and where there are fault lines in the Dales, then there are likely to be veins of valuable minerals such as lead, plus calcite, barytes etc.
Pockmarked hillside near Stump Cross
Looking almost like shell holes from an old battlefield, these dips and hollows are almost certainly the work of man. Note also the line of hollows running across the photo higher up. All these features are due to lead workings, the higher line following a vein across the moor. This area close to the B6265 is also close to the eastern end of the Craven fault zone, and where there are fault lines in the Dales, then there are likely to be veins of valuable minerals such as lead, plus calcite, barytes etc.
The stile for the path to Skyreholme The path leads past Troller's Gill
The stile for the path to Skyreholme
The path leads past Troller's Gill
The path to Skyreholme A lead mine can be seen in distance
The path to Skyreholme
A lead mine can be seen in distance
Old lead mine workings on path to Skyreholme
Old lead mine workings on path to Skyreholme
Face of the Troll (Barghest) in Trollers Gill Dry limestone gorge with the semblance of a face. Legend has it that a barghest (or barguest) in the form of a spectral black dog claimed a human victim, commemorated in a poem (1828).
Face of the Troll (Barghest) in Trollers Gill
Dry limestone gorge with the semblance of a face. Legend has it that a barghest (or barguest) in the form of a spectral black dog claimed a human victim, commemorated in a poem (1828).
B6265 towards Stump Cross Caverns Looking west along the B6265 towards the buildings at Stump Cross Caverns. Ahead is the bulk of Burnsall and Thorpe Fell, the 'pimples' to the right being small reef knoll limestone hills.
B6265 towards Stump Cross Caverns
Looking west along the B6265 towards the buildings at Stump Cross Caverns. Ahead is the bulk of Burnsall and Thorpe Fell, the 'pimples' to the right being small reef knoll limestone hills.
Across Appletreewick Pasture A Wharfedale view looking west towards the hidden course of the river and with Thorpe Fell in the distance. To the right of that are the small conical lumps that are the limestone reef knoll hills.
Across Appletreewick Pasture
A Wharfedale view looking west towards the hidden course of the river and with Thorpe Fell in the distance. To the right of that are the small conical lumps that are the limestone reef knoll hills.
The Hen The Hen and Chicks are a line of shafts that run WNW of the main open cut that is Gill Heads Vein. They date from the mid 18thC and were dug in the search for lead ore. They are large shafts, and this one is still open despite being covered with an assortment of rusty metal and tatty wire fencing.
The Hen
The Hen and Chicks are a line of shafts that run WNW of the main open cut that is Gill Heads Vein. They date from the mid 18thC and were dug in the search for lead ore. They are large shafts, and this one is still open despite being covered with an assortment of rusty metal and tatty wire fencing.
Nussey Green Lathe A roofless barn surrounded by wire cages, presumably for keeping game birds.
Nussey Green Lathe
A roofless barn surrounded by wire cages, presumably for keeping game birds.
Yorkshire  Dales  Sailing  Club  Grimwith  Reservoir The reservoir dam can be seen at the left, there is a 4.5 mile walk around the reservoir, far from the maddening crowds.
Yorkshire Dales Sailing Club Grimwith Reservoir
The reservoir dam can be seen at the left, there is a 4.5 mile walk around the reservoir, far from the maddening crowds.
Grimwith  Reservoir Access road off the B6265, a car park and picnic tables, separate from the sailing club. A walk around the reservoir is 4.5 miles
Grimwith Reservoir
Access road off the B6265, a car park and picnic tables, separate from the sailing club. A walk around the reservoir is 4.5 miles
Access  road  from  Grimworth  Reservoir  onto  B6265
Access road from Grimworth Reservoir onto B6265
Show me another place!

Appletreewick is located at Grid Ref: SE0763 (Lat: 54.069542, Lng: -1.892923)

Division: West Riding

Administrative County: North Yorkshire

District: Craven

Police Authority: North Yorkshire

What 3 Words

///luckier.bits.frightens. Near Grassington, North Yorkshire

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Nearby Amenities

Located within 500m of 54.069542,-1.892923
Grimwith Fell
Is In: UK,Yorkshire,North Yorkshire,Nidderdale
Is In Country: UK
Is In County: North Yorkshire
Is In Historical County: Yorkshire
Natural: fell
Source: NPE
Lat/Long: 54.0733704/-1.8891344
Historic: mine_shaft
Source: OS 1:25k
Lat/Long: 54.0680555/-1.8912295
Historic: mine_shaft
Source: OS 1:25k
Lat/Long: 54.0670447/-1.8884402
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0665486/-1.8981934
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0664449/-1.8978394
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0670682/-1.8988693
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0663756/-1.8983705
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0663599/-1.897539
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0666714/-1.8977804
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0697764/-1.8892375
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0693672/-1.8917803
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0686051/-1.8938295
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0702672/-1.8879715
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0686747/-1.8934861
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0691531/-1.8926386
Wood's Shaft
Historic: mine_shaft
Mineral: lead
Source: Bing
Source Name: Northern Mine Research Society
Lat/Long: 54.0681455/-1.8915979
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0689894/-1.8865553
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0702609/-1.8881003
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0680322/-1.8948702
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0686432/-1.8869845
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0685421/-1.8863085
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0686747/-1.8865768
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0697009/-1.8866411
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0680765/-1.8945054
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0696817/-1.8896881
Historic: mine_shaft
Source: Bing
Lat/Long: 54.070343/-1.8858258
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0680828/-1.8963615
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0682525/-1.8947092
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0683721/-1.887832
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0703238/-1.887596
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0699527/-1.8882397
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0698331/-1.8890444
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0679251/-1.8955139
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0690836/-1.8930999
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0702171/-1.8882505
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0697323/-1.8894521
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0690713/-1.8934325
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0703052/-1.8877569
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0703175/-1.8862549
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0691909/-1.8867377
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0686492/-1.8949774
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0700226/-1.8889386
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0699328/-1.8898774
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0695536/-1.8907572
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0658515/-1.8971247
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0697692/-1.8878201
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0658594/-1.8958855
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0697912/-1.8863369
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0696763/-1.8884987
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0658924/-1.8967197
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0657493/-1.8950506
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0690184/-1.8907196
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0695126/-1.8866641
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0697392/-1.8876592
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0697518/-1.8883003
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0695536/-1.8872944
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0691836/-1.8907142
Historic: mine_shaft
Source: Bing
Lat/Long: 54.069541/-1.8862752
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0710503/-1.8898051
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0709495/-1.8900894
Historic: mine_shaft
Source: Bing
Lat/Long: 54.067295/-1.8984204
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0707892/-1.8903255
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0672256/-1.8982648
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0673926/-1.8976586
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0678144/-1.8942683
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0671817/-1.8977766
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0678742/-1.8940108
Historic: mine_shaft
Source: OS 1:25k
Lat/Long: 54.0670037/-1.8888045
Grimwith Fell
Natural: peak
Source: OS 1:25k
Lat/Long: 54.0713525/-1.8898274
Croft Gill
Natural: valley
Source: OS 1853
Lat/Long: 54.0664007/-1.8921309
Croft Gill Lathe
Description: Former barn
Historic: archaeological_site
Source: OS 1853
Lat/Long: 54.0656452/-1.8904894
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0688783/-1.892868
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0688813/-1.8926588
Historic: mine_shaft
Source: OS 1894
Lat/Long: 54.0712142/-1.8968906
Historic: mine_shaft
Source: OS 1894
Lat/Long: 54.0711827/-1.8945635
Lamber
Historic: mine_shaft
Source: OS 1894
Source Name: Northern Mine Research Society
Lat/Long: 54.0732979/-1.8945849
Historic: mine_shaft
Source: OS 1894
Lat/Long: 54.0712079/-1.8953563
Historic: mine_shaft
Source: OS 1894
Lat/Long: 54.0737134/-1.8949932
Historic: mine_shaft
Source: OS 1894
Lat/Long: 54.0715727/-1.8939197
Lambert Shaft
Historic: mine_shaft
Source: OS 1894;Bing
Source Name: Northern Mine Research Society
Lat/Long: 54.0727373/-1.8940107
Whitaker's Level
Historic: mine_shaft
Mineral: lead
Source: Northern Mine Research Society;Bing
Lat/Long: 54.0662879/-1.8911421
Historic: mine_shaft
Source: Bing
Lat/Long: 54.0679153/-1.8912716
The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.

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