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The total area of the Exmoor National Park is 692.8 square kilometres (267.5 sq mi), of which 71% is in Somerset and 29% in Devon. The moor has given its name to a National Park, which includes the Brendon Hills, the East Lyn Valley, the Vale of Porlock and 55 kilometres (34 mi) of the Bristol Channel coast. Even more precisely Exmoor is defined as the remnant of the royal forest of 18,810 acres allotted to the king in 1815, equating to 12/22nds of the total, in acres 10,262 1/4, which was sold to John Knight (1765вЂ“1850) in 1818, which comprises the present Exmoor Parish, whose parish church is situated in Simonsbath. Exmoor is more precisely defined as the area of the former synonymous ancient royal hunting forest, officially surveyed 1815вЂ“1818 as 18,810 acres in extent. Other important mineral groups include the native elements, sulfides, oxides, halides, carbonates, sulfates, and phosphates.Exmoor is loosely defined as an area of hilly open moorland in west Somerset and north Devon in South West England, named after the River Exe the source of which is situated in the centre of the area, 2 miles NW of Simonsbath. These tetrahedra can be polymerized to give the subclasses: orthosilicates (no polymerization, thus single tetrahedra), disilicates (two tetrahedra bonded together), cyclosilicates (rings of tetrahedra), inosilicates (chains of tetrahedra), phyllosilicates (sheets of tetrahedra), and tectosilicates (three-dimensional network of tetrahedra). All silicate minerals have a base unit of a 4- silica tetrahedra-that is, a silicon cation coordinated by four oxygen anions, which gives the shape of a tetrahedron. The silicate class of minerals is subdivided into six subclasses by the degree of polymerization in the chemical structure. Minerals are classified by key chemical constituents the two dominant systems are the Dana classification and the Strunz classification.

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