Tarbat Ness: Difference between revisions

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{{county|Cromarty}}
[[File:Tarbet ness.jpg|right|thumb|300px|Tarbat Ness and its lighthouse]]
[[File:Tarbet ness.jpg|right|thumb|300px|Tarbat Ness and its lighthouse]]
'''Tarbat Ness''' is headland that lies at the end of the Tarbat peninsula on the [[North Sea]] coast of [[Easter Ross]], at the south of the entrance to the [[Dornoch Firth]]. This is a detached part of [[Cromartyshire]], encompassing the headland, the villages of [[Tarbat]] and [[Portmahomack]] and the coastland as far south as the latter.
'''Tarbat Ness''' is headland that lies at the end of the Tarbat peninsula on the [[North Sea]] coast of [[Easter Ross]], at the south of the entrance to the [[Dornoch Firth]]. The name of the headland is from the Gaelic ''tairbeart'' meaning "isthmus" and the Old Norse ''ness'', meaning "headland".<ref>Mac an Tailier (2003) p. 111</ref>


The name of the headland is from the Gaelic ''tairbeart'' meaning "isthmus" and the Old Norse ''ness'', meaning "headland".<ref>Mac an Tailier (2003) p. 111</ref>
This is a detached part of [[Cromartyshire]], the territory of that county encompassing the headland (with the hamlets of Wilkhaven and Bindal) and coming far south as [[Portmahomack]], though excluding the sands of Port Uilleim. It forms the easternmost point of the county.


==Geology and geomorphology==
==Geology and geomorphology==
The Upper Old Red Sandstone Devonian period bedrock contains fish fossils. There are examples of a range of pitting, saltspray and honeycomb erosion and "some of the best examples of differential erosion processes on tilted sandstone strata in Scotland".<ref>[http://www.tarbat-ness.ukfossils.co.uk/ Tarbat Ness]. UK Fossils. Retrieved 27 January 2014.</ref><ref name=Hansom>Hansom, J.D [http://www.jncc.gov.uk/page-2731 "Tarbat Ness"]. JNCC/''Geological Conservation Review''. Volume 28: Coastal Geomorphology of Great Britain. Chapter 3: Hard-rock cliffs.  Retrieved 27 January 2014.</ref>
The Upper Old Red Sandstone Devonian period bedrock contains fish fossils. There are examples of a range of pitting, saltspray and honeycomb erosion and "some of the best examples of differential erosion processes on tilted sandstone strata in Scotland".<ref>[http://www.tarbat-ness.ukfossils.co.uk/ Tarbat Ness]. UK Fossils. Retrieved 27 January 2014.</ref><ref name=Hansom>Hansom, J.D [http://www.jncc.gov.uk/page-2731 "Tarbat Ness"]. JNCC/''Geological Conservation Review''. Volume 28: Coastal Geomorphology of Great Britain. Chapter 3: Hard-rock cliffs.  Retrieved 27 January 2014.</ref>


The headland reaches {{convert|17|m|ft|0|x}} above sea level in the south and east and 35 feet in the north and west. The raised beaches provide evidence of the post -glacial changes in sea level. Water depths offshore reach 35 feet at 300 yards offshore and 65 feet at about 3 miles offshore.<ref name=Hansom/>
The headland reaches 56 feet above sea level in the south and east and 35 feet in the north and west. The raised beaches provide evidence of the post-glacial changes in sea level. Water depths offshore reach 35 feet at 300 yards offshore and 65 feet at about three miles offshore.<ref name=Hansom/>


==History==
==History==
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==References==
==References==
*Location map: {{wmap|57.86639|-3.77417|zoom=14}}
{{reflist}}
{{reflist}}


* {{citation | title=Lost Kingdoms: Celtic Scotland and the Middle Ages  |first=John Lenox | last=Roberts | publisher=Edinburgh University Press | year=1997 | isbn=978-0-7486-0910-9}}
* {{citation | title=Lost Kingdoms: Celtic Scotland and the Middle Ages  |first=John Lenox | last=Roberts | publisher=Edinburgh University Press | year=1997 | isbn=978-0-7486-0910-9}}
* Thomson, William P. L. (2008) ''The New History of Orkney''. Edinburgh. Birlinn. ISBN 978-1-84158-696-0
* Thomson, William P. L. (2008) ''The New History of Orkney''. Edinburgh. Birlinn. ISBN 978-1-84158-696-0
{{coord|57|51|59|N|3|46|27|W|type:landmark_region:GB_dim:2000|display=title}}


[[Category:Headlands of Cromartyshire]]
[[Category:Headlands of Cromartyshire]]
[[Category:Parcels of Cromartyshire]]
[[Category:Extreme points of Cromartyshire]]

Latest revision as of 12:53, 19 February 2017

Tarbat Ness and its lighthouse

Tarbat Ness is headland that lies at the end of the Tarbat peninsula on the North Sea coast of Easter Ross, at the south of the entrance to the Dornoch Firth. The name of the headland is from the Gaelic tairbeart meaning "isthmus" and the Old Norse ness, meaning "headland".[1]

This is a detached part of Cromartyshire, the territory of that county encompassing the headland (with the hamlets of Wilkhaven and Bindal) and coming far south as Portmahomack, though excluding the sands of Port Uilleim. It forms the easternmost point of the county.

Geology and geomorphology

The Upper Old Red Sandstone Devonian period bedrock contains fish fossils. There are examples of a range of pitting, saltspray and honeycomb erosion and "some of the best examples of differential erosion processes on tilted sandstone strata in Scotland".[2][3]

The headland reaches 56 feet above sea level in the south and east and 35 feet in the north and west. The raised beaches provide evidence of the post-glacial changes in sea level. Water depths offshore reach 35 feet at 300 yards offshore and 65 feet at about three miles offshore.[3]

History

1880 Ordnance Survey map

According to the Orkneyinga Saga the Earl of Orkney, Torf-Einarr "was the first man to dig peat for fuel, firewood being very scarce on the islands, at Tarbat Ness" (Torfness in the original).[4] This is said to explain his nickname, torf meaning "peat", but it is clearly an absurd assertion.[5]

At the Battle of Tarbat Ness in the 11th century, Thorfinn the Mighty defeated "Karl Hundason",[6] possibly a Viking name for Macbeth.

Further down the peninsula near the village of Portmahomack, in the 1480s the Clan Ross slaughtered a raiding party from the Clan Mackay by locking them in the Tarbat Old Church and setting fire to it. This event is known as the Battle of Tarbat.

On 14 October 1941 a Saro Lerwick flying boat assigned to No. 4 OTU L7268 crashed into the sea near Tarbat Ness following failure of the port engine. The aircraft could not maintain altitude on single engine. Six of the crew were killed, three recovered alive.[7]

Modern day

Tarbat Ness from the south across the Moray Firth

The Tarbat Ness Lighthouse stands at the northwest tip of the peninsula. It was built in 1830 by Robert Stevenson and has an elevation of 174 feet and 203 steps to the top of the tower.[8]

The restored Ballone Castle lies at the south east end of the peninsula north of the village of Rockfield.

References

  1. Mac an Tailier (2003) p. 111
  2. Tarbat Ness. UK Fossils. Retrieved 27 January 2014.
  3. 3.0 3.1 Hansom, J.D "Tarbat Ness". JNCC/Geological Conservation Review. Volume 28: Coastal Geomorphology of Great Britain. Chapter 3: Hard-rock cliffs. Retrieved 27 January 2014.
  4. Orkneyinga Saga (1981) Chapter 7. p. 29
  5. Thomson (2008) p. 37
  6. Roberts (1997) p. 22
  7. Bussy, Geoffrey, " 'Forgotten' Flying Boat: Saro's Unfortunate Lerwick", Air Enthusiast, Stamford, Lincs, UK, Number 124, July–August 2006, pp. 25, 27.
  8. "Tarbat Ness Lighthouse". Gazetteer for Scotland. Retrieved 27 January 2014.
  • Roberts, John Lenox (1997), Lost Kingdoms: Celtic Scotland and the Middle Ages, Edinburgh University Press, ISBN 978-0-7486-0910-9 
  • Thomson, William P. L. (2008) The New History of Orkney. Edinburgh. Birlinn. ISBN 978-1-84158-696-0