el mayor campo de picones de la isla

English translation: the largest area of cinder cones on the island

GLOSSARY ENTRY (DERIVED FROM QUESTION BELOW)
Spanish term or phrase:el mayor campo de picones de la isla
English translation:the largest area of cinder cones on the island
Entered by: Sidra

20:39 Dec 27, 2008
Spanish to English translations [PRO]
Tourism & Travel
Spanish term or phrase: el mayor campo de picones de la isla
El Pico es un cono de cínder de 574 metros de altura, con cráter en herradura abierto al Noroeste. Emitió gran cantidad de materiales, originando junto con el cercano volcán del Monte Lentiscal, contemporáneo suyo, el mayor campo de picones de la isla, utilizado desde el siglo XVIII para el cultivo de la vid.
Sidra
Brazil
Local time: 19:41
the largest area of cinder cones on the island
Explanation:
does this help ?
EVOLUTION OF A COMPLEX CINDER CONE, RED MOUNTAIN, ARIZONA - [ Traduire cette page ]Red Mountain (RM) is an ~740 ka cinder cone located near the NE edge of the San Francisco volcanic field in northern AZ. RM underwent phases of both ...
gsa.confex.com/gsa/2004AM/finalprogram/abstract_73917.htm - 6k - En cache - Pages similaires

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Note added at 8 mins (2008-12-27 20:48:27 GMT)
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Geography of Lanzarote

Lanzarote, the northernmost and – together with Fuerteventura – also the easternmost of the Canary Islands, is located only 125 km (77 miles) from the African mainland. It is the fourth largest island of the archipelago and has an actual population of around 108.000 inhabitants. Its surface covers 846 sq. kilometres (326 sq. miles) and only 21 kilometres (13 miles) separate the west from the east coast at its widest point, which means that it can easily be crossed in short car journeys. Geographically, Lanzarote belongs to Macaronesia, a group of islands in the Atlantic including the Canary Islands as well as the archipelagos of Madeira, the Azores and Cape Verde.

Lanzarote is a contrasting desert island of volcanic origin, with largely predominating lava fields. It has a long history of volcanic eruptions and almost every type of rock found on the island is of volcanic origin.

The ‘Island of the 1000 volcanoes’ – as it is frequently called – is despite its high number of volcanic peaks – it boasts around 300 - the least mountainous of the archipelago, with its highest mount – the volcano Peñas del Chache near Haría in the northern part of the island – reaching 670 m (2,198 ft) above sea level. Its interior is barren, reminiscent of a lunar landscape, covered with volcanic massifs and plains, dotted with small craters and cones and amorphous eruptive rock formations.

Lanzarote is the island of the Canary archipelago, which is most dominated - physically and culturally – by its dormant volcanic power. The well-documented Timanfaya eruptions between 1730 and 1736 were the longest lasting and most powerful periods of volcanic activity ever known. They devastated two thirds of the island – almost the whole southern part – creating a blackened, lifeless malpaís (badlands) of cinders, ash and lava, at the same time considerably increasing the surface of the island, with lava flows running into the sea. Although the oldest sediments, dating from 60 million years ago, indicate there was movement deep in the ocean, which permitted the Canaries to arise, it was eruptions from 15 million years ago, from which Lanzarote was formed like it is known today. The last eruptions, which lasted only two months, took place in 1824 in the same area as the ones from a hundred years before.

The landscapes of Lanzarote clearly demonstrate the usual volcanic process of a single major cone creating a number of smaller cones all around as outlets for gases and liquids. Lanzarote also boasts some fine examples of lava tubes – one has 7.5 km (4.7 miles) and is considered one of the longest in the world – and large caverns formed by gas explosions, some of which have collapsed (for good examples visit Cueva de los Verdes and Jameos del Agua).

Although some eruptions on the island occurred already thousands of years ago, the extremely dry climate and the erosion caused by strong winds explain the fact that vast badlands areas are still devoid of almost any vegetationre
Selected response from:

ormiston
Local time: 00:41
Grading comment
This helps me quite alot! Thanks a bunchful!
4 KudoZ points were awarded for this answer



Summary of answers provided
4the largest rolling hills field in the island
Gilberto Diaz Castro
4the largest cone field on the island
Carol Gullidge
3the largest area of cinder cones on the island
ormiston


  

Answers


6 mins   confidence: Answerer confidence 3/5Answerer confidence 3/5
the largest area of cinder cones on the island


Explanation:
does this help ?
EVOLUTION OF A COMPLEX CINDER CONE, RED MOUNTAIN, ARIZONA - [ Traduire cette page ]Red Mountain (RM) is an ~740 ka cinder cone located near the NE edge of the San Francisco volcanic field in northern AZ. RM underwent phases of both ...
gsa.confex.com/gsa/2004AM/finalprogram/abstract_73917.htm - 6k - En cache - Pages similaires

--------------------------------------------------
Note added at 8 mins (2008-12-27 20:48:27 GMT)
--------------------------------------------------

Geography of Lanzarote

Lanzarote, the northernmost and – together with Fuerteventura – also the easternmost of the Canary Islands, is located only 125 km (77 miles) from the African mainland. It is the fourth largest island of the archipelago and has an actual population of around 108.000 inhabitants. Its surface covers 846 sq. kilometres (326 sq. miles) and only 21 kilometres (13 miles) separate the west from the east coast at its widest point, which means that it can easily be crossed in short car journeys. Geographically, Lanzarote belongs to Macaronesia, a group of islands in the Atlantic including the Canary Islands as well as the archipelagos of Madeira, the Azores and Cape Verde.

Lanzarote is a contrasting desert island of volcanic origin, with largely predominating lava fields. It has a long history of volcanic eruptions and almost every type of rock found on the island is of volcanic origin.

The ‘Island of the 1000 volcanoes’ – as it is frequently called – is despite its high number of volcanic peaks – it boasts around 300 - the least mountainous of the archipelago, with its highest mount – the volcano Peñas del Chache near Haría in the northern part of the island – reaching 670 m (2,198 ft) above sea level. Its interior is barren, reminiscent of a lunar landscape, covered with volcanic massifs and plains, dotted with small craters and cones and amorphous eruptive rock formations.

Lanzarote is the island of the Canary archipelago, which is most dominated - physically and culturally – by its dormant volcanic power. The well-documented Timanfaya eruptions between 1730 and 1736 were the longest lasting and most powerful periods of volcanic activity ever known. They devastated two thirds of the island – almost the whole southern part – creating a blackened, lifeless malpaís (badlands) of cinders, ash and lava, at the same time considerably increasing the surface of the island, with lava flows running into the sea. Although the oldest sediments, dating from 60 million years ago, indicate there was movement deep in the ocean, which permitted the Canaries to arise, it was eruptions from 15 million years ago, from which Lanzarote was formed like it is known today. The last eruptions, which lasted only two months, took place in 1824 in the same area as the ones from a hundred years before.

The landscapes of Lanzarote clearly demonstrate the usual volcanic process of a single major cone creating a number of smaller cones all around as outlets for gases and liquids. Lanzarote also boasts some fine examples of lava tubes – one has 7.5 km (4.7 miles) and is considered one of the longest in the world – and large caverns formed by gas explosions, some of which have collapsed (for good examples visit Cueva de los Verdes and Jameos del Agua).

Although some eruptions on the island occurred already thousands of years ago, the extremely dry climate and the erosion caused by strong winds explain the fact that vast badlands areas are still devoid of almost any vegetationre

ormiston
Local time: 00:41
Specializes in field
Native speaker of: English
PRO pts in category: 32
Grading comment
This helps me quite alot! Thanks a bunchful!
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24 mins   confidence: Answerer confidence 4/5Answerer confidence 4/5
the largest rolling hills field in the island


Explanation:
It describes a landscape that provides great opportunities for harvesting grapes. Grapes don't grow in high mountains but on rolling hills that provide for good irrigation without holding excess water that could harm them.

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Note added at 34 mins (2008-12-27 21:14:26 GMT)
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Una foto lo dice todo...

http://www.panoramio.com/photo/13649071
http://www.centralcoastmag.com/html/gourmet/wine/001_fieldsf...
http://www.dreamstime.com/fall-colors-in-grape-field-image66...
http://www.flickr.com/photos/tferey/61565849/
http://www.handtomouth.net/JVS/Img/Landscape_Vineyards.jpg

Gilberto Diaz Castro
United States
Local time: 18:41
Works in field
Native speaker of: Native in EnglishEnglish, Native in SpanishSpanish
PRO pts in category: 4

Peer comments on this answer (and responses from the answerer)
neutral  Carol Gullidge: sorry Gilberto, but I don't think there's such a thing as a rolling hills field :)//G: I have nothing against vineyards, but can't see what the link is between these, nice as they are, with "campo de picones"/Couldn't find "picones" using EDIT :(
40 mins
  -> Would you please read the complete text provided? It states that the land of these "Picones" has been dedicated to grow grapes, or did I mis read the context provided?
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1 hr   confidence: Answerer confidence 4/5Answerer confidence 4/5
the largest cone field on the island


Explanation:
I'm normally wary of direct translations, but this seems to be what it's called:

Boron concentrations of volcanic fields in different geotectonic ...... Volcanic Belt (Ceboruco Cone Field), which is associated with recent subduction. ... The average B content of the Tenerife (Canary Islands) samples ( 6.4 ...
cat.inist.fr/?aModele=afficheN&cpsidt=18450339 -
Similar pages

by K GMELING - 2007 - Cited by 1 - Related articles - All 5 versions
Journal of Volcanology and Geothermal Research : Boron ...Tenerife, Canary Island; 2.3. Waipiata volcanic field, New Zealand; 2.4. Mexico/ Pinacate and Ceboruco cone field. 3. Samples and experimental technique; 4. ...
linkinghub.elsevier.com/retrieve/pii/S0377027306003039 - Similar pages

by K Gm ling - 2007 - Cited by 1 - Related articles
Lithos : A geochemical transect across a heterogeneous mantle ...Other examples include the Canary Islands (Hoernle et al., ... 4000 m to a subaerial cinder cone field located near Madeira's capital Funchal. ...
linkinghub.elsevier.com/retrieve/pii/S0024493706000491 -
Similar pages
by J Geldmacher - 2006 - Cited by 1 - Related articles

COSIS.net - Poster Programme - NH9.04 Multidisciplinary approaches ...Susceptibility analysis of basaltic eruptions at Tenerife (Canary Islands) ... advances in remote sensing: the case of Mauna Kea shield's cone field ...
www.cosis.net/members/meetings/sessions/poster_programme.ph... - 45k - Cached - Similar pages

April 2002 Archive - News Headlines - Willamette University...

The Quaternary Volcanic Fields of the East and West Eifel (Germany)nineties in the Eifel, Sicily and the Canaries and Madeira led to the postu- .... scoria cone field (mostly ca. 0.1 - <5 million years) (Connor and Conway ...

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Note added at 1 hr (2008-12-27 22:16:41 GMT)
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This is oibviously wrong, viz K Donnelly's answer to a subsequent question.

...black porous volcanic grains, known as lapilli (picon in Lanzarote)
www.vulkaner.no/t/lanza/cactus.html


My answer should now read:

The largest picón/lapilli field on the island

Whether you choose picón or lapilli (or whether you gloss) depends on the target audience

Carol Gullidge
United Kingdom
Local time: 23:41
Specializes in field
Native speaker of: Native in EnglishEnglish
PRO pts in category: 180
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