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[[Image:Hawk's Tor.jpg|thumb|right|250px|Hawk's Tor, on [[Bodmin Moor]]]]
<!--schweizbezogen-->
{{otheruses}}
{{Infobox Ort in der Schweiz
A '''tor''' is a type of [[rock (geology)|rock]] outcrop formed by [[weathering]], usually found on or near the summit of a [[hill]]. In the [[South West England|South West]] of [[England]], where the term originated, it is also a word used for the hills themselves — particularly the high points of [[Dartmoor]], in [[Devon]], and [[Bodmin Moor]], in [[Cornwall]]. The word Tor is also used across the [[Bristol Channel]] in southern [[Wales]], particularly on the rocky coastlines such as the [[Vale of Glamorgan]] and the [[Gower Peninsula]]; on the Gower one of the sandy beaches near [[Oxwich Bay]] is called 'Tor Bay' because the beach is framed by a huge outcrop of [[carboniferous]] [[limestone]]. The term is notable for being, along with ''[[crag]]'', one among a mere handful of [[Celtic languages| Celtic]] loan-words ([[Old Welsh]] ''twrr'', [[Scottish Gaelic language|Scots Gaelic]] ''tòrr''), primarily of a geographic or topographical nature, to be borrowed into vernacular English prior to the modern era.
|NAME_ORT = Robasacco
|BILDPFAD_KARTE =
|BILDPFAD_WAPPEN =
|BILD =
|REGION-ISO = CH-TI
|BEZIRK = [[Bezirk Bellinzona]]
|KREIS = [[Kreis Giubiasco]]
|GEMEINDE = Cadenazzo
|PLZ = 6599
|UN/LOCODE = CH RCT
|BREITENGRAD = 46.143056
|LÄNGENGRAD = 8.945833
|HÖHE = 492
|FLÄCHE = 2.78
|EINWOHNER = 109
|STAND_EINWOHNER = 31. Dezember 2007
|WEBSITE =
}}
'''Robasacco''' war bis zum 14. März 2005 eine [[politische Gemeinde]] im [[Kreis Giubiasco]], im [[Bezirk Bellinzona]] des Kantons [[Kanton Tessin|Tessin]] in der Schweiz.


==Formation==
== Die alte Komunanz ==
Millions of years ago magma created deep-seated dome batholiths which over time were revealed to the atmosphere and allowed for weathering to break down its composition forming tors.
Die Komunanz Medeglia/Robasacco fusioniert mit Komunanz Cadenazzo/Monteceneri seit 1. Januar 2004<ref>[http://www.bfs.admin.ch/bfs/portal/de/index/infothek/nomenklaturen/blank/blank/gem_liste/03.Document.112644.pdf Amtliches Gemeindeverzeichnis der Schweiz] auf www.bfs.admin.ch</ref>.


Tors are composed usually of [[granite]] (although [[Devonian]] and [[Carboniferous]] outcrops are also found), though occasionally of other hard rocks such as [[quartzite]], and are the result of millions of years of [[weathering]]. In prehistoric times, when the land was covered in forest, rain water seeped into the ground and gradually weathered the bedrock through its natural cracks, or joints. Once the land became exposed, the weathering was accelerated, particularly during the [[Ice Age]] when freezing water expanded in the cracks. The result can be seen today in dramatic rock formations.
== Sehenswürdigkeiten ==
* Pfarrkirche San Leonardo, erwähnt 1205<ref>Simona Martinoli et alii: ''Guida d’arte della Svizzera italiana.'', Hrsg. [[Gesellschaft für Schweizerische Kunstgeschichte]], Edizioni Casagrande, Bellinzona 2007, ISBN 978-88-7713-482-0, 50.</ref>
* Betkapelle della Madonna
* Zwei andere Betkapellen
* Fresko mit Sonnenuhr auf der Fassade eines alten Bauernhaus
* Alter Saumpfad Munscendrin<ref>[http://www.precassino.ch/uploads/PDF/LeVieDeiBriganti_IT.pdf Le vie dei briganti] (italienisch)</ref>.


Weathering has also given rise to circular ‘rock basins’, formed by the accumulation of water and the repeated freezing and thawing — a fine example is to be found at [[Kes Tor]].
== Literatur ==
* [[Virgilio Gilardoni]]: ''Inventario delle cose d’arte e di antichità.'', Band II, Distretto di Bellinzona, Edizioni dello Stato, Bellinzona 1955, S. 268-270.
* Virgilio Gilardoni: ''Il Romanico. Catalogo dei monumenti nella Repubblica e Cantone del Ticino.'', La Vesconta, Casagrande S.A., Bellinzona 1967, S. 527.
* Bernhard Anderes: ''Guida d’Arte della Svizzera Italiana.'', Edizioni Trelingue, Porza-Lugano 1980, S. 26.
* Flavio Maggi: ''Patriziati e patrizi ticinesi.'', Pramo Edizioni, Viganello 1997.
* Simona Martinoli et alii: ''Guida d’arte della Svizzera italiana.'', Edizioni Casagrande, Bellinzona 2007.


As the weathering of the tors continues, the rock is broken down into ever smaller sizes. Many hillsides are covered with loose rocks, known as clitter, which have provided ready building materials for thousands of years. Eventually the granite is weathered down to a level equivalent to sandy [[gravel]], known as growan, which consists of individual crystals.
== Weblinks ==
* [http://www.cadenazzo.ch/ Website der Gemeinde Cadenazzo]
* [http://www.ti.ch/CAN/SegGC/comunicazioni/GC/odg-mes/rapporti/5567-r.htm Historiche Nachrichten und Begründung der neue Gemeinde] (italienisch)
* [http://www4.ti.ch/dt/dstm/sst/ubc/temi/inventario-dei-beni-culturali/consultazione/consultazione/ Robasacco: Kulturgüterinventar des Kantons Tessin]


{{sectstub}}
== Einzelnachweise ==
<references/>


==Tors on Dartmoor==
[[Kategorie:Ort im Kanton Tessin]]

[[Kategorie:Ehemalige politische Gemeinde in der Schweiz]]
Dartmoor represents one of the largest areas of exposed [[granite]] in the [[United Kingdom]], covering an area of 241 square miles (625 square kilometres) (source: Dartmoor National Park). It is part of a chain of granite stretching through [[Cornwall]], as far as the [[Isles of Scilly]].

Some of the more durable granite survived to form the rocky crowns of Dartmoor tors. One of the best known is at [[Hay Tor]], on the eastern part of the moor, whose granite is of unusually fine quality and was quarried during the [[19th century|19th]] and early [[20th century|20th]] centuries. Its stone was used to construct the pillars outside the [[British Museum]] in [[London]], and to build [[London Bridge]] (now in [[Arizona]]). The last granite to be quarried there was used to build [[Exeter]] War Memorial in [[1919]].

[[Ten Tors]] is an annual weekend hike on Dartmoor

==Highest tors on Dartmoor==
*[[High Willhays]] (621m) N.B. This is not a Tor, Just the highest point
*[[Yes Tor]] (619m)
*Hangingstone Hill (603m)
*Great Links Tor (586m)
*Kitty Tor (578m)
*Fur Tor (572m)
*Great Kneeset (567m)
*Higher Dunnagoat Tor (560m)
*Hunt Tor (560m)
*Cosdon Beacon (550m)
*Lower Dunnagoat Tor (550m)
*Dinger Tor (550m)
*Devils Tor (549m)
*Rough Tor (547m)
*West Mill Tor (541m)
*Flat Tor (540m)
*Chat Tor (540m)
*Green Tor (540m)
*Steng-a-Tor (540m)

==Other well-known Dartmoor tors==
*[[Fox Tor]] (190m)
*[[Hay Tor]] (457m)
*[[Hound Tor]] (414m)
*[[Kes Tor]] (437m)
*[[Sheeps Tor]] (369m)

[[Image:Higger Tor 14-04-06.jpg|200px|right|thumb|Higger Tor in the [[Peak District]].]]
==Other tors==
*Black Tor, Derwent Edge (538m)
*Dovestone Tor, Derwent Edge (505m)
*[[Glastonbury Tor]]
*Great Tor, Bamford
*Howshaw Tor
*Ladybower Tor
*Low tor
*[[Mam Tor]] (517m)
*[[Shining Tor]]
*[[Over Owler Tor]] (375m)
*[[Higger Tor]] (384m)
*Whinstone Lee Tor
*White Tor, Derwent Moors (487m)
*The Barns of Bynack, Granite tors on [[Bynack More]] in the [[Cairngorms]]
*The Salt Cellar, Gritstone tor on [[Derwent Edge]] in the [[Peak District]]

==See also==
{{Commons|Category:Tors|Tors}}
*[[List of peaks of the Peak District]]
*[http://www.richkni.co.uk/dartmoor/tors.htm Pictures of Dartmoor tors]

[[Category:Dartmoor]]
[[Category:Derbyshire]]
[[Category:Geography of Cornwall]]
[[Category:Geography of Devon]]
[[Category:Geology of England]]
[[Category:West Country]]

[[de:Felsnadel]]

Version vom 12. November 2006, 20:50 Uhr

Hawk's Tor, on Bodmin Moor

Vorlage:Otheruses A tor is a type of rock outcrop formed by weathering, usually found on or near the summit of a hill. In the South West of England, where the term originated, it is also a word used for the hills themselves — particularly the high points of Dartmoor, in Devon, and Bodmin Moor, in Cornwall. The word Tor is also used across the Bristol Channel in southern Wales, particularly on the rocky coastlines such as the Vale of Glamorgan and the Gower Peninsula; on the Gower one of the sandy beaches near Oxwich Bay is called 'Tor Bay' because the beach is framed by a huge outcrop of carboniferous limestone. The term is notable for being, along with crag, one among a mere handful of Celtic loan-words (Old Welsh twrr, Scots Gaelic tòrr), primarily of a geographic or topographical nature, to be borrowed into vernacular English prior to the modern era.

Formation

Millions of years ago magma created deep-seated dome batholiths which over time were revealed to the atmosphere and allowed for weathering to break down its composition forming tors.

Tors are composed usually of granite (although Devonian and Carboniferous outcrops are also found), though occasionally of other hard rocks such as quartzite, and are the result of millions of years of weathering. In prehistoric times, when the land was covered in forest, rain water seeped into the ground and gradually weathered the bedrock through its natural cracks, or joints. Once the land became exposed, the weathering was accelerated, particularly during the Ice Age when freezing water expanded in the cracks. The result can be seen today in dramatic rock formations.

Weathering has also given rise to circular ‘rock basins’, formed by the accumulation of water and the repeated freezing and thawing — a fine example is to be found at Kes Tor.

As the weathering of the tors continues, the rock is broken down into ever smaller sizes. Many hillsides are covered with loose rocks, known as clitter, which have provided ready building materials for thousands of years. Eventually the granite is weathered down to a level equivalent to sandy gravel, known as growan, which consists of individual crystals.

Vorlage:Sectstub

Tors on Dartmoor

Dartmoor represents one of the largest areas of exposed granite in the United Kingdom, covering an area of 241 square miles (625 square kilometres) (source: Dartmoor National Park). It is part of a chain of granite stretching through Cornwall, as far as the Isles of Scilly.

Some of the more durable granite survived to form the rocky crowns of Dartmoor tors. One of the best known is at Hay Tor, on the eastern part of the moor, whose granite is of unusually fine quality and was quarried during the 19th and early 20th centuries. Its stone was used to construct the pillars outside the British Museum in London, and to build London Bridge (now in Arizona). The last granite to be quarried there was used to build Exeter War Memorial in 1919.

Ten Tors is an annual weekend hike on Dartmoor

Highest tors on Dartmoor

  • High Willhays (621m) N.B. This is not a Tor, Just the highest point
  • Yes Tor (619m)
  • Hangingstone Hill (603m)
  • Great Links Tor (586m)
  • Kitty Tor (578m)
  • Fur Tor (572m)
  • Great Kneeset (567m)
  • Higher Dunnagoat Tor (560m)
  • Hunt Tor (560m)
  • Cosdon Beacon (550m)
  • Lower Dunnagoat Tor (550m)
  • Dinger Tor (550m)
  • Devils Tor (549m)
  • Rough Tor (547m)
  • West Mill Tor (541m)
  • Flat Tor (540m)
  • Chat Tor (540m)
  • Green Tor (540m)
  • Steng-a-Tor (540m)

Other well-known Dartmoor tors

Higger Tor in the Peak District.

Other tors

See also

Commons: Tors – Album mit Bildern, Videos und Audiodateien

de:Felsnadel