Formation of lava fields on Lanzarote

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Discussion Overview

The discussion revolves around the geological features and formation processes of lava fields in Lanzarote, particularly focusing on the characteristics of the surface structures, the types of volcanic materials present, and the nature of the beaches in the area. Participants explore various aspects of volcanic geology, including the formation of a'a lava, lapilli, and the impact of environmental conditions on the landscape.

Discussion Character

  • Exploratory
  • Technical explanation
  • Conceptual clarification
  • Debate/contested

Main Points Raised

  • One participant describes the surface of the lava field as having large broken fragments and air gaps, questioning the mechanism that caused these features to rise above the ground level.
  • Another suggests that the lava could be a'a lava, which cools in a blocky manner, and discusses the potential for the dunes to be made of pumice or scoria, noting their lightness and ability to be moved by wind.
  • A participant mentions the term lapilli, suggesting that the small stones observed may be pyroclastic materials, and discusses the geological differences between Lanzarote and Tenerife regarding vegetation and rainfall.
  • There is curiosity about the origin of the golden sand on the beaches, with questions raised about whether it could be artificial or derived from surrounding geological materials.
  • Another participant speculates on the possibility that the surrounding rocks could be lighter in color but weathered to appear dark, prompting inquiries about the composition of the beach sand.
  • One participant expresses a desire to approach the landscape with a geologist's perspective in future explorations, indicating a learning process through the discussion.

Areas of Agreement / Disagreement

Participants express various hypotheses regarding the geological features and materials, but no consensus is reached on the specific mechanisms or origins of the observed phenomena. The discussion remains open-ended with multiple competing views and uncertainties.

Contextual Notes

Participants mention limitations in available geological maps and the challenges of accessing certain areas, which may affect the understanding of the geological context. There is also uncertainty regarding the classification of the beach sand and the geological history of the region.

Who May Find This Useful

Individuals interested in volcanic geology, landscape formation, and the environmental conditions of Lanzarote may find this discussion informative.

sophiecentaur
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Just got back from Lanzarote and was walking through a recent (300yr old Timenfaya) lava field. Very little rain in 300 years so it's more or less like it started, I guess. A great landscape to investigate the way volcanic landscapes develop.
What I couldn't understand was the structure of the surface in places. It looked as if a giant JCB had been breaking up turning over a layer of concrete - or possibly a plough in a clay field. The surface consisted of large broken fragments (many, at least a metre diameter), with lots of air gaps underneath. I couldn't figure out what mechanism lifted the lumps so far above the mean ground level. The field was more or less horizontal so it wasn't as if they had rolled downhill or been carried like the lumps of granite in Snowdonia etc.

Also, there seemed to be dunes of fine stones - a la Sahara but the wind would need to have been v. strong to form them with such large particles.

Someone must have worked it out. . . . .
 
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Photos would be haelpful if you have them.

The lava sounds like a'a lava. It cools in a blocky manner and the solid bits get shifted and tossed about by the parts still flowing. Have a look here: http://www.universetoday.com/guide-to-space/earth/aa-lava/

The dunes of stones could be pumice or scoria: (formerly) airbourne volcanic pebbles that rain down on the landscape after being thrown out of the volcano. They'd be very bubbly in texture and if pumice, so light they'll float on water. I'd bet small pumice stones could be blown about by the wind. Don't rule out them being water deposited though.

I've been to Tenerife, a couple of islands over. Fascinating landscapes, eh?
 
Thanks for that.
Yes, I heard the term a'a lava used. Also, they referred to the small stones as pilli (spelling?). They are more dense than pumice but have holes in them which are used in systems to catch the dew in the morning; Lanzarote has humid air at times but very little rain.
Lanzarote has so little water that the 16k year old lava fields are pretty much unchanged, with just a thin layer of vegetation in places. I believe Tenerife has much more rain and loads of vegetation so changes are much more rapid.
Here are two photos I took.
Some of it's like Mars apart from the blue sky. Strange.
 

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Lapilli, maybe? http://en.wikipedia.org/wiki/Lapilli
They definitely sound pyroclastic.

Tenerife gets lots of rain in the lower altitudes but up on top of the volcano past the treeline it's more like that in the photos.
 
Lapilli - that's the badger. So, it's just stayed there for 300yrs. It certainly brings the idea of Geological Time into perspective.
Another strange thing. Many of the beaches seem to have typical golden / white sand on them despite all the surrounding cliffs and rocks being very black. These are natural beaches, in inaccessible coves, so the sand can't have been introduced artificially. Where does it come from and why isn't there more sign of black grains in it as on other island beaches? The sea is knocking hell out of the coast all the time!
Compare the two pictures, taken not many km apart. (I am quite pleased with the 'surf and golden sand' picture')
 

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Are there any acidic igneous rocks on Lanzarote? I haven't been able to find a geological map. Can you be sure the beach isn't artificial?
 
I can't say about the geology ( hence my questions) but I can say that a lot of small golden coves are remote and almost inaccessible. The surf beach in the photo is on La Graciosa which is small an non-trippery and there aren't even Tarmac roads. Rocks all seem very black, though. I guess this question applies all round coasts, with some exceptions like S Devon.
 
Tough one. Perhaps the surrounding rocks were light rocks but with a dark weathered surface. Did you see the colour of any freshly broken bits? Did you have a close look at the grains? Were they rocky particles, or fragments of broken shell?
 
I clearly walked around the place with Engineer's eyes open rather than Geologist's. NExt time, if the re is one, I shall bear in mind your questions, matthyaouw. Thanks for your answers, though. I a a bit wiser about things than I was!
 
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