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Vebraalto.Com St Geroges House Pickering North Yorkshire YO18 7AE Tel: 01751 472724 Email: [email protected] www.boultoncooper.co.uk Sunset Cottage Wapping Lane, Great Edstone, York, YO62 6PD Offers In Excess Of £365,000 A highly individual village house situated in a quiet and secluded part of this peaceful Ryedale village located approximately two miles south of Kirkbymoorside. The house occupies large gardens and grounds extending to approximately 1/2 acre. Access is gained from Wapping Lane in the centre of the village with the far end boundary facing onto the main approach road to the village. There is significant development potential on this part of the site for those who might wish to explore it (planning potential on this part of the site for those who might wish to explore it (planning consultation has been undertaken). The residence, which is believed to have been converted from a pair of cottages provides spacious three bedroom accommodation with two principal reception rooms all facing westerly overlooking the extensive and well maintained garden. The house has appealing elevations and provides a rare opportunity to acquire a village property 'with a bit of difference'. General upgrading should be anticipated and there is good scope to extend if more living space is required. Good garage and parking space is included. Great Edstone is a peaceful village located in the Vale of Pickering and to the south of Kirkbymoorside well away from any principal routes or thoroughfares. Excellent facilities are available in Kirkbymoorside and other nearby market town and the boundary of the North York Moors National Park lies within a ten minute drive. Entrance Hall Dining/Living Room 16'7" x 6'9" (5.06m x 2.06m) 14'0" x 13'3" (4.27m x 4.06m) Front facing Upvc window, outer door to garden, traditional staircase to first floor with understairs cupboard, radiator. Shower Room 6'7" x 6'2" (2.01m x 1.88m) Fully tiled walls, wash basin and vanity unit, w.c., shower cubicle, radiator. Sitting Room 25'5" x 14'9" (7.75m x 4.52m) Well proportioned room overlooking the garden with sliding doors opening onto patio, radiator. First Floor Landing With Radiator and fitted cupboard. Two rear facing windows. Bedroom One 14'7" x 13'6" (4.45m x 4.12m) A large main reception room with two front facing Gable window and front facing window overlooking the Upvc windows overlooking the garden and further side garden, radiator and fitted wardrobes. facing window, three radiators, chimney breast, open Bedroom Two fire in stone surround and side features. 15'1" x 15'3" (4.6m x 4.65m) Kitchen A spacious double room with gable and front facing 14'2" x 10'5" (4.32m x 3.2m) windows, two radiators. Bedroom Three 10'0" x 11'6" (3.05m x 3.51m) A small double sized room with window overlooking the garden and radiator. Bathroom 10'0" x 6'7" (3.07m x 2.03m) With window overlooking the garden, bath, w.c., bidet, wash basin in stand, tiled walls and radiator. Boiler House With Mistral Oil fired boiler. Gardens and Grounds A small yard lies to one side with useful workshop and stores 25' x 8'10" (7.62m x 2.69m). Constructed of brick under a tiled roof. Garage and Parking Area With space for several vehicles Rear facing window and door to side entrance porch. Extensive base units incorporating dishwasher, plumbing for washer, electric oven and hob, matching wall mounted cabinets and full height fridge freezer unit. Two radiators, arched opening to dining/living room. Gardens Services mains, water, drainage, electricity are connected. Oil fired central heating. EPC Band F Full details available to view at our Kirkbymoorside Office. Council Tax We have been verbally informed that this property lies in Band F The extensive gardens and grounds are a particular feature of the property. Local Authority The mature garden with the well established shrub and Ryedale District Council, Ryedale House, Malton, Tel: tree borders providing complete seclusion. The garden 01653 600666. is laid out with a series of lawns and flagged footpaths with extensive shrub and flower beds, hedging and Viewing orchard. The far end adjoins the main road leading into Strictly by appointment through the agents. Tel: the village, with potential for a separate access. There 01751 432792 is also an excellent aspect overlooking the vale of Pickering and towards the distant North York Moors. Planning A pre application consultation process has been undertaken with the local planning authority. The response to the proposal suggests that an area of the garden joining the western boundary would receive favourable consideration for residential development of up to three dwellings. A local occupancy restriction would apply. This is an informal, but informed opinion only and is not a planning consent. Details are available on request. .
Recommended publications
  • Yorkshire's Hidden Vale Area
    YORKSHIRE’S HIDDEN VALE The roles of the River Derwent and the River Hertford in Landscape Action for the Eastern Vale of Pickering A report by Bowles Green Ltd and The Yorkshire Wildlife Trust With generous support from LEADER Coast, Wolds, Wetlands and Waterways (CWWW) through the East Riding and North Yorkshire Waterways Partnership; The Rural Development Programme for England/LEADER East Riding of Yorkshire 1 Acknowledgements This report would not have been possible without the generous grant from LEADER Coast, Wolds, Wetlands and Waterways (CWWW) via the East Riding and North Yorkshire Waterways Partnership. The authors would also like to thank Harriet Linfoot for her hard work in the local communities, gathering the essential information which shaped this report. Over 200 people provided responses to face to face questions or the on-line survey. Their honest engagement made this report possible and worthwhile. A large number of people commented on the draft of this report and others unselfishly allowed their works and writings to be used or quoted. To all these people, our grateful thanks. Cover photograph Flixton Brow view from the top of the escarpment across the Valley ©Tim Burkinshaw Senior Authors Yorkshire Wildlife Trust Kevin Bayes Harriet Linfoot Bowles Green Steven Green Judith Bowles 2 Contents page 1.0 Summary 5 2.0 Introduction to the document 7 3.0 Introduction to Yorkshire’s Hidden Vale 8 4.0 Background documents on Landscape and Significance 9 5.0 Programme Area 10 6.0 The Cultural and Natural Heritage of the Programme
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  • Documentary Records of Floods in the Vale of Pickering
    Documentary records of floods in the Vale of Pickering These records are taken from the British Hydrological Society Chronology of Hydrological Events. As they are documentary records, their content is partly a function of the recording of events coupled to the extent to which documents have been found. However, they show a notable phenomenon, often found in other flood records, of a flood rich period in the late-nineteenth century followed by a flood poor period in the early 20 th century. There then follows the textual descriptions that accompanies each flood. Figure 1. Dates of documented flood records before 1950. Note that these are documented which means that they are not equivalent to the continual record of a water level recorder and reflect time-varying trends in the extent to which documents were recorded. 1750 1770 1790 1810 1830 1850 1870 1890 1910 1930 1950 " A sudden inundation of the river Rye happened at Helmsley in Yorkshire, such as had never been known by the oldest people in those parts, probably occasioned by the late heavy rains.Two houses were entirely washed away , the one inhabited by James Holdforth, he and his whole family drowned, except his wife, who being sick in her bed, was carried down the stream half a mile, and at last washed off into a field, where she was found the next morning very little hurt. The other house belonged to John Sunley, was also drowned, and all his family. In the whole thirteen persons.(sic) Two other houses were greatly damaged, as was also the stone bridge at the entrance to the town; fourteen hay-stacks were driven down the river a mile, on one of which was a half year old calf, who kept its footing, and was taken off alive.
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  • 1 Diamicton from the Vale of Pickering and Tabular Hills, North
    Diamicton from the Vale of Pickering and Tabular Hills, north-east Yorkshire: evidence for a Middle Pleistocene (MIS8) glaciation? John H. Powell, Jonathan R. Ford and James B. Riding 1British Geological Survey, Keyworth, Nottingham, NG12 5GG, United Kingdom *Corresponding author: e-mail: [email protected] (J.H. Powell) ABSTRACT Diamicton deposits (up to 6.90 m thick) in the Vale of Pickering and the Tabular Hills (North York Moors) have been confirmed by cored boreholes. The diamicton is interpreted as glacial till with a matrix consisting predominantly of grey-brown, yellow-brown and dark grey, stiff to very stiff clay and sandy clay with occasional thin beds of laminated sand and clay. Sub-rounded to sub-angular erratic clasts were sourced predominantly from local Upper Jurassic Corallian Group bedrock exposed in the southern part of the North York Moors. Clasts include well-rounded, pebbles of Jurassic sandstone, mudstone and sparse Jurassic coal derived from outcrops on the North York Moors. Fragments of underlying Upper Jurassic mudstone bedrock form the predominant clasts in the lower part of the till. The paucity of exotic clasts and a local derivation suggests a relatively small glacier - perhaps a temperate-plateau ice-field, was established on the Tabular Hills. The glacier subsequently advanced southwards to the Vale of Pickering depositing locally derived subglacial traction till at the base, passing up to lodgement till. Local preservation of the degraded till outcrops in the Vale of Pickering, the overconsolidated nature of the clay till matrix, striated pebbles and the presence of sub-rounded pebbles suggests deposition during a glacial cold stage post-MIS 12 (Anglian) and pre-MIS 2 (Devensian).
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  • North Yorkshire Moors and Cleveland Hills
    Character Area North Yorkshire Moors 25 and Cleveland Hills Key Characteristics Landscape Character ● Upland plateau landscape underlain mainly by The North York Moors and Cleveland Hills are a very sandstone and mudstone of Middle Jurassic age and, clearly demarcated block of high land in the north east of in the south, calcareous sandstone and limestone of the counties of Yorkshire and Cleveland. To the north-east Upper Jurassic age, with areas of undulating land the boundary is the North Sea while to the north and west arising from deposits of glacial till, sand and gravel. there is a steep scarp slope rising above the Tees valley and the Vale of Mowbray. Here a curiously shaped, conical ● Plateaux dissected by a series of dales, often broad outlier of Lower Jurassic rocks, Roseberry Topping, has and sweeping but with steep-sided river valleys in become a distinctive and well-known landmark. The places, floored by Lower Jurassic shales. Cleveland Hills are the highest area but they merge into the ● Extensive areas of heather moorland on plateaux and hills, Hambleton Hills in the south-west which in turn drop creating a sense of space, expansiveness and openness. sharply down to the Vale of York. Along the south margin the Tabular Hills dip gently to the south and east but there ● Arable landscape to south and east, but pasture on is still a distinct change in slope where the land drops down elevated, sweeping plateaux and hills. to the Vale of Pickering. ● Sparsely settled, with population concentrated in the dales and around the fringes.
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  • The Corallian of the Vale of Pickering, Yorkshire
    Baseline groundwater chemistry: the Corallian of the Vale of Pickering, Yorkshire Groundwater Programme Open Report OR/15/048 BRITISH GEOLOGICAL SURVEY GROUNDWATER PROGRAMME OPEN REPORT OR/15/048 Baseline groundwater chemistry: The National Grid and other the Corallian of the Vale of Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Pickering, Yorkshire Stationery Office. Licence No: 100017897/ 2015. Keywords Baseline, water quality, aquifer, J. M. Bearcock, P.L. Smedley, and C. J. Milne England, trace elements, pollution. Contributor Front cover Cleave Dike Quarry, Hambleton K. J. Griffiths Hills [SE 507 863], looking south-east. The thick-bedded unit at the base of the face is the lower leaf of the Hambleton Oolite. The overlying Birdsall Calcareous Grit forms the upper two-thirds of the face. (Photograph: G. Moore) Bibliographical reference BEARCOCK, J.M., SMEDLEY, P.L., AND MILNE, C.J.. 2015. Baseline groundwater chemistry: the Corallian of the Vale of Pickering, Yorkshire. British Geological Survey Open Report, OR/15/048. 70pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. Maps and diagrams in this book use topography based on Ordnance Survey mapping.
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  • Archaeological Excavations in Sherburn, Vale of Pickering, North Yorkshire
    Archaeological Excavations in Sherburn, Vale of Pickering, North Yorkshire. September 2011 The village of Sherburn, situated on the southern side of the eastern end of the Vale of Pickering and overlooked by the Yorkshire Wolds to the south, is the largest of the villages that occupy the sandy margin between the foot of the Yorkshire Wolds and the former wetlands that characterise the eastern end of the Vale. A royal vill with two churches, identified in Domesday, the village sits astride the Wykeham-Sherburn moraine which survives as a slight ridge projecting into the former wetlands which in antiquity served as a route across the Vale. The surviving church, which was almost completely rebuilt between 1909 and 1912, incorporates a number of fragments of Late Saxon/Viking Age sculptural stone in the present fabric. The church sits in a dominant position at the northern end of the present village. Archaeological research by the Landscape Research Centre over the last three decades has included extensive air-photographic survey and, more recently, large scale geophysical survey around the present village. The geophysical survey in particular reveals that Sherburn has a settlement history that extends back into later prehistory, and that during the Anglo- Saxon period the settlement extended over more than 25ha, larger than the excavated village at West Heslerton, but with a considerably larger number and greater density of Grubenhäuser, the distinctive cavity floor buildings that characterise settlements of the Early and Middle Anglo-Saxon periods. Two discoveries, one made through regular aerial survey over the last 30 years and another made during the mid 19th century, are the subject of a small research programme designed to try and understand Sherburn’s role during the Anglo-Saxon period.
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  • Vale of Pickering Statement of Significance
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  • EGU2018-1093, 2018 EGU General Assembly 2018 © Author(S) 2017
    Geophysical Research Abstracts Vol. 20, EGU2018-1093, 2018 EGU General Assembly 2018 © Author(s) 2017. CC Attribution 4.0 license. Late Glacial Environments within the Vale of Pickering, North Yorkshire, UK Laura Eddey (1), Mark Bateman (1), Stephen Livingstone (1), and Jonathan Lee (2) (1) Department of Geography, University of Sheffield, Sheffield, UK, S10 2TN , (2) British Geological Survey, Keyworth, Nottingham, NG12 5GG During the Late Devensian, the Vale of Pickering in North Yorkshire, UK is thought to have been the site of a large proglacial lake dammed by the North Sea Ice Lobe of the British and Irish Ice sheet (BIIS) to the east and the Vale of York Lobe to the west. Lake levels are reported to have reached between 70 and 30 m O.D. (Kendall, 1902; Edwards, 1978; Foster, 1985; Evans et al., 2017) based on field evidence. But, controversy remained as to what lake levels were attained and when, and how lake levels were affected by the surrounding North Sea and Vale of York Ice. Here, we present flood fills from high-resolution Digital Terrain Models (DTMs) adjusted for isostatic de- pression; glacial geomorphological mapping, sedimentary analysis and 21 new optically stimulated luminescence (OSL) dates. We show that there are multiple iterations of Lake Pickering, with the higher lake level (70 m O.D.) reported by Kendall (1902) existing prior to (>30 ka) the LGM. Fluctuations in lake levels were controlled by the dynamics of both the North Sea Lobe and the Vale of York Lobe as well as the presence of high-stage Glacial Lake Humber (Bateman et al., 2017).
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  • Broats Farm Salton Near Kirkbymoorside, York, North Yorkshire
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  • Statement of Physical Characteristics and Agricultural Land Classification
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  • Vale of Pickering Statement of Significance
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  • The Old School House, Ganton, North Yorkshire
    The Old School House, Ganton, North Yorkshire 2 The Old School House, Station Road, Ganton Offers Based on £525,000 AN EXTREMELEY RARE OPPORTUNITY TO PURCHASE A SUBSTANTIAL AND HIGHLY INDIVIDUAL DETACHED FORMER SCHOOL HOUSE SITUATED IN A PRIME LOCATION ADJACENT TO AND OVERLOOKING THE FAMOUS GANTON GOLF COURSE. Situated in the Vale of Pickering between York and Scarborough, The Old School House is a deceptively spacious detached residence that offers well-proportioned accommodation that oozes character and charm. At comfortably over 3,000 sq. ft.(excluding the garage) the property lends itself to use as a family home or country retreat as well as offering the opportunity for the creation of a luxury B&B facility for golfers, shooting enthusiasts, walkers and the many other visitors to this most attractive part of North Yorkshire. The centrally heated and partly double glazed accommodation includes up to six bedrooms, four bathrooms and three reception rooms as well as a kitchen with four oven Aga, utility room and cloakroom. York 32 Miles ~ Scarborough 10 Miles ~ Malton 15 miles ~ Beverley 27 miles ~ Hull 38 Miles ~ A1(M) 56 miles Situation It was also the venue of the Ryder Cup in 1949, and Lounge 22’6” x 18’ (6.86m x 5.49m) The Old School House occupies a plot of a little over half rather more recently The Walker Cup in 2003 when the With open fire having a Baxi grate set within a traditional an acre with a lawned frontage onto the attractive white GB and Ireland team was victorious for a historic third fireplace, dado rail, two double radiators, four wall light post lined access road that leads to the golf club.
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