Tankerness

Tankerness is a district in the St Andrews parish in Mainland, Orkney, Scotland. Essentially a peninsula, it is about 13km south-east of Kirkwall and 1km east of Kirkwall Airport. The origin of the place name is uncertain, but it may derive from the Norse personal name "Tannskári". A "ness" is a promontory. GeographyTankerness is bounded to the north and west by Inganess Bay, to the east by Deer Sound, and to the south by the A960. Inganess Bay and Deer Sound meet at the prominent headland of Rerwick Head. Loch of Tankerness, which is just under 1km2 in size, lies in the central area. The landscape is more gentle than the hilly terrain to the west and is fertile farmland. Bordering Inganess Bay is the Long Ayre, a kilometer-long gravel tombolo enclosing a tidal pool. GeologyThe Tankerness peninsula is underlain by Rousay flagstones, an Old Red Sandstone of Middle Devonian age, that were deposited in Lake Orcadie. These lacustrine rocks were laid down when the land that now forms Orkney was 16 degrees south of the equator within the Southern Hemisphere's desert belt. The flagstones show a marked cyclicity in their sedimentation, which is interpreted as representing regular climatically driven changes in lake level caused by Milankovitch cyclicity.

Tankerness is a district in the St Andrews parish in Mainland, Orkney, Scotland. Essentially a peninsula, it is about 13km south-east of Kirkwall and 1km east of Kirkwall Airport. The origin of the place name is uncertain, but it may derive from the Norse personal name "Tannskári". A "ness" is a promontory. GeographyTankerness is bounded to the north and west by Inganess Bay, to the east by Deer Sound, and to the south by the A960. Inganess Bay and Deer Sound meet at the prominent headland of Rerwick Head. Loch of Tankerness, which is just under 1km2 in size, lies in the central area. The landscape is more gentle than the hilly terrain to the west and is fertile farmland. Bordering Inganess Bay is the Long Ayre, a kilometer-long gravel tombolo enclosing a tidal pool. GeologyThe Tankerness peninsula is underlain by Rousay flagstones, an Old Red Sandstone of Middle Devonian age, that were deposited in Lake Orcadie. These lacustrine rocks were laid down when the land that now forms Orkney was 16 degrees south of the equator within the Southern Hemisphere's desert belt. The flagstones show a marked cyclicity in their sedimentation, which is interpreted as representing regular climatically driven changes in lake level caused by Milankovitch cyclicity.