Doug Shepherd's photos with the keyword: Vale of Mowbray

The view from Sutton Bank is to the west and the market town of Thirsk, about 6 miles/9.5 km away (hidden by the haze). The Vale of York (left of picture) becomes the Vale of Mowbray to the north of Thirsk (right of picture) The road leading into the picture is the A170 which runs from Thirsk to Scarborough via Pickering, a distance of 47 miles/76 km. The Vale of York is often said to stretch from the River Tees in the north to the Humber Estuary in the south. More properly it is just the central part of this area which is truly the Vale of York, with the Vale of Mowbray to its north and the Humberhead Levels to its south. It is bounded by the Howardian Hills and Yorkshire Wolds to the east and the Pennines to the west. The low-lying ridge of the Escrick moraine marks its southern boundary. The city of York lies in the centre of the area. The Vale of Mowbray (sometimes mistakenly referred to as the Vale of York) is a stretch of low-lying land between the North York Moors and the Hambleton Hills to the east and the Yorkshire Dales to the west. To the north lie the Cleveland lowlands and to the south, in the region of Thirsk, the Vale of Mowbray becomes the Vale of York proper. At Sutton Bank the A170 road runs up the bank with a maximum gradient of 1 in 4 (25%), and includes several tight bends as well as a hairpin bend. The road rises 520 feet (160 m) in under 1 mile (1.6 km) in this section.

The Hambleton Hills and Vale of Mowbray from Roulston Scar (Sutton Bank) The view is to the north 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 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 (400 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. The example below is displayed at Helmsley Castle 13 miles (20 km) to the east. Sutton Bank (also known as Roulston Scar) is a high point on the Hambleton Hills with extensive views over the Vale of York and the Vale of Mowbray. The hill is the site of one of the most important prehistoric monuments in the region, an Iron Age hill fort built in around 400 BC. The Hambleton Drove Road runs along the summit of the hills, it is part of an ancient highway running from Scotland to the south of England. It is thought to be prehistoric and various burial grounds from the Neolithic and Bronze Ages are evident along its route. Large-scale movement of cattle from Scotland to market in England during the 18th and 19th centuries have given it the name by which it is known today.