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#485 | |
"Erling B."
Dec 2005
23·11 Posts |
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Last fiddled with by japelprime on 2021-03-23 at 00:19 |
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#486 | |
Feb 2017
Nowhere
22·1,117 Posts |
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But how did they determine that it was that long ago? That's what I'm asking. I read that the last eruption on the peninsula was after human settlement, and was a different volcano. So the last eruption of Fagradals Mountain was before that. Something is saying that the basalt from the last eruption of Fagradals Mountain is 6000 to 7000 years old, and not 3000 years old or 10000 years old. What? |
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#487 |
Romulan Interpreter
Jun 2011
Thailand
2×32×521 Posts |
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#488 | |
1976 Toyota Corona years forever!
"Wayne"
Nov 2006
Saskatchewan, Canada
10001111110012 Posts |
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![]() Last fiddled with by petrw1 on 2021-03-23 at 14:14 |
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#489 | |
Feb 2017
Nowhere
22·1,117 Posts |
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EDIT: (update) I did see Páll Einarsson, an emeritus Professor of Geophysics, University of Iceland, named as a source in some of the news reports. I'm guessing he told the reporters how long the volcano had been dormant. The last eruption on the Reykjanes Peninsula was 781 years ago. That's in recorded history. Some of the news reports muffed that, saying that the Fagradals Mountain volcano (the one currently erupting) had erupted 781 years ago. Further update: Professor Einarsson has kindly informed me that the last lava flows around Fagradals before the current eruption were dated by C14 and "tephrochronology," the dating of ash flows deposited on top of the lava flows. He also sent me a 20-plus page paper from JÖKULL No. 58, 2008 which looks to be interesting reading. Last fiddled with by Dr Sardonicus on 2021-03-25 at 13:05 Reason: As indicated |
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#490 | |
"Erling B."
Dec 2005
8810 Posts |
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#491 |
"Erling B."
Dec 2005
23×11 Posts |
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But this tells you only The dept of where the material is coming from. How they know the time ? When geologists digs through the earth layers they are counting the years in the different layers finding this ashes in the layers from that periode of time.
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#492 |
Bamboozled!
"𒉺𒌌𒇷𒆷𒀭"
May 2003
Down not across
1064610 Posts |
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I don't know but can think of several possibilities. Each could be used on either the material in question or material with similar chemistry, in particular with similar isotopic concentrations.
Endogenous methods include measuring the amount of decay products of U and Th since the material was last liquid. Until then the concentrations of each will be independent of the chemical composition of the bulk. Afterwards, the different minerals will (I believe, I don't know) be different in each mineral. That solidification starts the clock ticking. Similarly, magnetism induced by the Earth's magnetic field will be frozen in both direction and intensity at the time of solidification. We have pretty good estimates for where the terrestrial field has been for rather a long time. Exogenous methods applicable to surface deposits include counting cosmic ray tracks or measuring erosion evidence, whether by rainfall or by abrasion. There are doubtless other possibilities. |
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