This is a list of lakes and tarns in North Yorkshire, England. Unlike the nearby Lake District, North Yorkshire does not have many natural lakes due to the porosity of the limestone underneath the surface. [1] [2] The JNCC Special Area of Conservation status for the Craven Limestone Complex lists running and standing Water at only 1%. [3] Upland tarns are common where the underlying stone allows the water to collect. These tarns are usually surrounded by peat, so most have relatively acidic water in comparison to the alkaline nature of water which runs over Limestone common in the area. [4]
Man-made reservoirs and dams, such as at Moss Dam in Swaledale, are not included, as the list focuses only on natural lakes and tarns. [5] The list only covers those within Yorkshire, and sites such as Sunbiggin Tarn, whilst in the Yorkshire Dales National Park, are not included, as that body of water is in the county of Cumbria. Some tarns or lakes may no longer exist; historical documents refer to Giggleswick and Wigglesworth as having tarns - however, these have either dried up or have been drained. [6]
Name | Location | Coordinates | Height AMSL | Volume | Notes | Ref |
---|---|---|---|---|---|---|
Birkdale Tarn | Keld | 54°24′40″N2°13′44″W / 54.411°N 2.229°W | 1,598 feet (487 m) | 11,900,000 cubic feet (336,000 m3) | [7] [8] | |
Birks Tarn | Birks Fell | 54°10′44″N2°07′12″W / 54.179°N 2.120°W | 1,959 feet (597 m) | 2,960,400 cubic feet (83,828 m3) | In the 1890s, Birks Tarn was described as being "two sheets of water", but would become one big body of water in heavy rains. | [9] [10] |
Cotter End Tarn | Cotterdale | 54°20′17″N2°16′48″W / 54.338°N 2.280°W | 1,696 feet (517 m) | [11] | ||
Cray Tarn | Oughtershaw | 54°13′34″N2°07′16″W / 54.226°N 2.121°W | 1,962 feet (598 m) | [12] | ||
Eshton Tarn | Bell Busk | 54°00′52″N2°07′37″W / 54.0145°N 2.127°W | 472 feet (144 m) | 1,519,100 cubic feet (43,015 m3) | [13] | |
Fleet Moss Tarn | Fleet Moss | 54°14′49″N2°11′38″W / 54.247°N 2.194°W | 1,896 feet (578 m) | [14] | ||
Fountains Fell Tarn | Fountains Fell | 54°08′13″N2°12′07″W / 54.137°N 2.202°W | 2,116 feet (645 m) | 3,000,000 cubic feet (86,000 m3) | [15] | |
Gallaber Pond (Flash) | Hellifield | 54°00′40″N2°14′17″W / 54.011°N 2.238°W | 490 feet (150 m) | The flash lake is sandwiched between the A65 road and the railway line north of Hellifield railway station. It does not appear on mapping from the early 1900s and is listed as a flash lake. | [16] | |
Gormire Lake | Sutton Bank | 54°14′31″N1°13′44″W / 54.242°N 1.229°W | 509 feet (155 m) | 5,500,000 cubic feet (155,000 m3) | Gormire has no major inflow, or outflow of water, and is thought to be fed by natural springs. | [17] [18] [19] |
Greensett Moss | Ribblehead | 54°14′02″N2°23′42″W / 54.234°N 2.395°W | 584 metres (1,916 ft) | 48,836 cubic metres (1,724,600 cu ft) | [20] [21] | |
Hunters Hole | Oughtershaw | 54°13′37″N2°07′55″W / 54.227°N 2.132°W | 2,057 feet (627 m) | [22] | ||
Locker Tarn | Carperby | 54°19′12″N1°59′49″W / 54.320°N 1.997°W | 1,086 feet (331 m) | 2,509,900 cubic feet (71,073 m3) | [23] [8] | |
Malham Tarn | Malhamdale | 54°05′49″N2°09′47″W / 54.097°N 2.163°W | 1,230 feet (375 m) | 55,066,300 cubic feet (1,559,303 m3) | [24] | |
Middle Tongue Tarn | Oughtershaw | 54°13′59″N2°08′31″W / 54.233°N 2.142°W | 2,047 feet (624 m) | The name derives from the fact that its straddles "the tongue [of land] of two valleys" | [25] [26] [27] | |
Newhouses Tarn | Horton-in-Ribblesdale | 54°10′08″N2°18′29″W / 54.169°N 2.308°W | 814 feet (248 m) | 2,340,000 cubic feet (66,261 m3) | Adjacent to the River Ribble. Listed on the lakes portal as "Unnamed Water Body ID 29701" and on OS Mapping as The Tarn. One book source from 1921 describes a tarn "1.5 miles (2.4 km)" north of Horton-in-Ribblesdale as "Newhouses Tarn", named after the nearest hamlet. | [28] [29] |
Oughtershaw Tarn | Oughtershaw | 54°14′02″N2°10′52″W / 54.234°N 2.181°W | 1,824 feet (556 m) | [30] | ||
Priest's Tarn | Grassington | 54°07′16″N1°57′32″W / 54.121°N 1.959°W | 1,691 feet (515.5 m) | [31] [32] | ||
Scarborough Mere | Scarborough | 54°15′40″N0°24′43″W / 54.261°N 0.412°W | 141 feet (43 m) | 9,895,300 cubic feet (280,205 m3) | [33] | |
Semerwater | Countersett | 54°16′48″N2°07′26″W / 54.280°N 2.124°W | 807 feet (246 m) | 35,327,800 cubic feet (1,000,372 m3) | [34] | |
Slatepit Moss | Ravenseat Moor | 54°26′17″N2°13′16″W / 54.438°N 2.221°W | 1,877 feet (572 m) | [35] | ||
South Grain Tarn | Oughtershaw | 54°13′52″N2°06′47″W / 54.231°N 2.113°W | 1,926 feet (587 m) | [36] | ||
Summer Lodge Tarn | Crackpot | 54°21′00″N2°04′41″W / 54.350°N 2.078°W | 1,722 feet (525 m) | 4,229,000 cubic feet (119,760 m3) | [37] [38] [8] | |
Whitaside Tarn | Crackpot | 54°21′04″N2°02′10″W / 54.351°N 2.036°W | 1,732 feet (528 m) | [39] | ||
Widdale Little Tarn [note 1] | Widdale Fell | 54°17′17″N2°19′05″W / 54.288°N 2.318°W | 2,090 feet (637 m) | [41] [42] |
Malham Cove is a large curved limestone formation 0.6 miles (1 km) north of the village of Malham, North Yorkshire, England. It was formed by a waterfall carrying meltwater from glaciers at the end of the last Ice Age more than 12,000 years ago. Today it is a well-known beauty spot and rock climbing crag within the Yorkshire Dales National Park. A large limestone pavement lies above the cove.
The Yorkshire Dales is an upland area of the Pennines in the historic county of Yorkshire, England, most of it in the Yorkshire Dales National Park created in 1954.
The Yorkshire Dales National Park is a 2,178 km2 (841 sq mi) national park in England covering most of the Yorkshire Dales, with the notable exception of Nidderdale. Most of the park is in North Yorkshire, with a sizeable area in Cumbria and a small part in Lancashire. The park was designated in 1954, and extended in 2016. Over 95% of the land in the Park is under private ownership; there are over 1,000 farms in this area.
Malham is a village and civil parish in the Craven district of North Yorkshire, England. Before 20th century boundary changes, the village was part of the Settle Rural District, in the historic West Riding of Yorkshire. In the Domesday Book, the name is given as Malgun, meaning "settlement by the gravelly places". In 2001 the parish had a population of approximately 150. Malham parish increased in size geographically and so at the 2011 Census had a population of 238.
Malham Tarn is a glacial lake near the village of Malham in the Yorkshire Dales, England. The lake is one of only eight upland alkaline lakes in Europe. At an altitude of 377 metres (1,237 ft) above sea level it is the highest marl lake in the United Kingdom. Its geology, flora and fauna have led to it being listed under a number of conservation designations. The site is currently owned by the National Trust, who used to lease part of the site to the Field Studies Council but this closed as a field centre in 2022. The site was the inspiration for Charles Kingsley's 1863 novel The Water-Babies, A Fairy Tale for a Land Baby.
Airton is a small village and civil parish in the Craven district of North Yorkshire, England, situated 10 miles (16 km) north-west of Skipton. The village had a population of 175 according to the 2001 Census, 228 at the 2011 Census, decreasing to 227 at the 2021 Census.
Gayle is a hamlet sited 0.4-mile (0.64 km) south of Hawes in Wensleydale, North Yorkshire, England. The hamlet is noted for the beck that flows through it and the old mill, which featured on the BBC programme Restoration.
Dentdale is a dale or valley in the north-west of the Yorkshire Dales National Park in Cumbria, England. It is the valley of the River Dee, but takes its name from the village of Dent. The dale runs east to west, starting at Dent Head, which is the location of a railway viaduct on the Settle-Carlisle Line.
Cogra Moss is a shallow reservoir to the east of the village of Lamplugh on the western edge of the English Lake District. It was created by the damming of Rakegill Beck in about 1880, though its function as a water supply ceased in 1975. The reservoir, which is surrounded by forestry plantations on three sides, is popular with walkers and anglers.
Ponden Reservoir is an artificial upland lake in the Worth Valley, near Stanbury, West Yorkshire, England. Ponden was built as a compensation reservoir after the nearby Watersheddles Reservoir (upstream) was used to divert water away from the River Worth. Ponden was needed to regulate the flow of water down the river into the downstream mills in the valley.
The Worth Valley is a geographic area in West Yorkshire, England, that extends eastwards from Crow Hill and Oxenhope Moor, providing drainage for the River Worth for nearly 10 miles (16 km) to the River Aire. It is a side valley to Airedale, with the River Worth being a major tributary of the River Aire. The Worth Valley was important for its contribution to the textiles industry of the West Riding of Yorkshire and was furnished with several reservoirs to allow mills to operate within the valley. Most of the reservoirs are still in use into the modern day.
Watersheddles Reservoir is an upland artificial lake in Lancashire, England. The reservoir was opened in 1877 by the Keighley Corporation Water Works, and is now owned by Yorkshire Water. It supplies water to the Worth Valley and Keighley area and compounds several streams at the source of the River Worth.
Fleet Moss is a upland area separating Wharfedale from Wensleydale in North Yorkshire, England. The area is 1,850 ft (560 m) above sea level. Fleet Moss is noted for its peat blanket bog, which has been dated to the Neolithic period. The area is ombrotrophic; this means it needs rain, hail snow and fog for its nutrients. Fleet Moss is known as the most eroded blanket bog in all of Yorkshire; because of its observable damage, it is known colloquially as The Somme, and as such, is visible from space.
Upper Barden Reservoir is an upland fresh water reservoir, one of two reservoirs that collect water from Barden Moor, and dam Barden Beck, a tributary of the River Wharfe in the Yorkshire Dales, North Yorkshire, England. The reservoir was opened in 1882 and also supplies fresh water to the Nidd Aqueduct, which transports it to Bradford. Upper Barden Reservoir was the second of the reservoirs to be built,.
Crummackdale,, is a small valley north of the village of Austwick in the Craven District of North Yorkshire, England. The Valley is drained by Austwick Beck, which flows into the River Wenning, which in turn heads westwards to empty into the Irish Sea. Crummackdale is a narrow south west facing dale, at the south west corner of the Yorkshire Dales National Park.
Fountains Fell Tarn, is an upland lake between the two peaks of Fountains Fell, in North Yorkshire, England. The tarn is close to the Pennine Way, some 4.3 miles (7 km) north west of Malham Tarn, and 4.3 miles (7 km) east of Horton in Ribblesdale. Water from the tarn flows eastwards through Cowside Beck, which is a tributary of the River Skirfare in Littondale. Whilst the water in the lake is acidic, as it runs off the mountain, it flows over Yoredale beds limestone and so becomes a harder water.
Priest's Tarn is an upland lake on Grassington Moor, in North Yorkshire, England. The water from Priest's Tarn was historically used for hydraulic mining purposes during the lead industry on Grassington Moor. The flow of water largely exits the hill to the south-east into Grimwith Reservoir, which in turn feeds into the River Wharfe. Walkers have observed that the tarn is looking like it is drying up.
Snaizeholme is a small side valley of Wensleydale in the Yorkshire Dales National Park (YDNP), North Yorkshire, England. The valley is noted for its red squirrel reserve, the only place within the North Yorkshire part of the Yorkshire Dales National Park where red squirrels are known to live, and a tree re-wilding project.