Hambleton Hills

The Hambleton Hills are a range of hills in North Yorkshire, England. They form the western edge of the North York Moors but are separated from the moors by the valley of the River Rye. They are the eastern boundary of the low-lying Vale of Mowbray which they abut with a precipitous escarpment. They run in a north–south direction for about 15 miles (24 km) and merge with the Cleveland Hills in the north and Howardian Hills in the south. The entire range is within the North York Moors National Park. The hills are made up of rocks of middle and late Jurassic age with the hard Corallian Limestone forming the cap at the highest points. The highest point is Black Hambleton which rises to 1,308 feet (399 m) at the northern end of the range. Roulston Scar reaches 919 feet (280 m) and Whitestone cliff is 1,063 feet (324 m). The Corallian Limestone also outcrops along the southern edge of the North York Moors forming the Tabular Hills which run from Black Hambleton eastwards to Scarborough, although much broken through by river valleys. In the 12th and 13th centuries, the Hambleton Hills was the production centre for York Glazed Ware, a type of Medieval ceramic.

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Yorkshire Gliding Club

The Yorkshire Gliding Club (YGC) operate from an airfield on Sutton Bank in the North York Moors National Park, England. The airfield site is 7 miles (11 km) east of Thirsk along the A170 road and just south of the National Park visitors centre at Sutton Bank. The club formed in 1934 from an amalgamation of gliding concerns from the West Riding of Yorkshire and has been in existence for over 80 years and has had many famous fliers such as Nicholas Goodhart, Amy Johnson and Fred Slingsby. The club's location, on top of Roulston Scar and Sutton Bank over the White Horse of Kilburn, and the sheer drop away of the cliff, has made it a notable aircraft launching point. It is the most popular gliding club in the north of England.

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Hood Abbey

Hood Abbey was an abbey on the grounds of today's Hood Grange, North Yorkshire, England. The abbey at Hood was known to be in existence as a hermitage since before 1138 when Roger de Mowbray granted it to a group of Savignian monks, who stayed for five years before relocating to Byland Abbey. After this, it was inhabited by monks from the Bridlington area who came west to take over Roger de Mowbray's newest priory at Newburgh. The site was dissolved in the 16th century, and all that remains are two windows incorporated into one of the barns which now occupy the site.

Gormire Lake

Gormire Lake is a natural lowland lake that lies at the foot of Whitestone Cliff, a western escarpment of the Hambleton Hills in the North York Moors National Park. The lake is 1.2 miles (2 km) east of the village of Sutton-under-Whitestonecliffe in North Yorkshire, England. Gormire has no inflow or major outflow of water. It is thought to be fed by an underground spring and drained by a limestone channel so the water finds a way out through the base of the cliff face to the east of the lake. The lake is also known as the White Mere, Lake Gormire, or more simply, Gormire. The name Gormire translates as filthy swamp. The lake was formed over 20,000 years ago by glacial erosion. When an ice sheet pushed its way between the Pennines and the North York Moors, it bulldozed the soft earth away and carved the cliffs at Whitestone and in turn the mud left over stopped the water's egress and formed the glacial lake. Gormire Lake was a result of this process and is fourth largest of the natural lakes in Yorkshire (the other three being Hornsea Mere, Malham Tarn and Semerwater). The lake was first designated as an Site of Special Scientific Interest (SSSI) in 1954; however, in 1985 the area surrounding the lake was incorporated into the SSSI status with the new area being 133.5 acres (54.03 ha). The new designation incorporates the broadleaf woodlands of Garbutt Wood which encroach right up to the water's edge. The lake is the setting of several myths; one being of a knight known as Sir Harry Scriven who conned the Abbot of Rievaulx Abbey into letting him ride his horse (a white mare, the so called derivation of White Mare Cliff (another name for Whitestonecliff)). The knight and the abbot rode on from an inn and as they did so, it turned into a race. The abbot then changed into the devil, which caused such panic in the knight that he couldn't stop the horse and himself plunging into Gormire Lake from the clifftop. The 'devil' was then seen to jump into the lake after them and the boiling effect of the devil in the water is what is said to have caused the darkness of the lake to this day. Other myths are that the lake is bottomless, that the bottom of the lake is the entrance to hell, there is submerged village underneath the water and that a goose once disappeared in the lake to emerge in a well at Kirkbymoorside stripped of all its feathers. Gormire Lake is popular with wild swimmers as it has no streams feeding it so there is very little current and the waters are described as being 'warm'. Swimmers have reported that it is seething with leeches. The Times named the lake as one of the 20 best lakes and rivers in Britain for wild swimming.

Hood Grange

Hood Grange is a hamlet and civil parish in the county of North Yorkshire, England. The population was less than 100 in the 2011 Census, so details are included in the civil parish of Sutton-under-Whitestonecliffe. The population of the parish was estimated at 10 in 2015. From 1974 to 2023 it was part of the district of Hambleton, it is now administered by the unitary North Yorkshire Council. It is located near Thirsk at the foot of Sutton Bank, south of the larger village of Sutton-under-Whitestonecliffe and next to Hood Hill, which is to the south. It is notable for consisting of only a single household after its population decreased rapidly in the late 19th century. Hood Grange has existed as a civil parish since 1866, prior to which the area was part of Kilburn. A monastery known as Hood Abbey existed here from before 1138 until its dissolution in the 16th century.