Deluge of Atlantis

Deluge of Atlantis
Deluge of Atlantis

Sunday, August 21, 2011

Youngest-Dryas Age Vulcanism in Central Europe and the North Atlantic

Dryas-age (Final Ice Age) Volcanic Bomb from Fayal, Azores (Wikipedia) Some of these are reported as dredged up from the ocean bed and consistently date as having erupted between 12000 and 8000 BC or 14000 to 10000 years ago.Lava has to be flung into the air (above water) to have this shape and texture.



Map showing Youngest Dryas and Earliest Postglacial volcanic ash in Central Europe and the North Atlantic. Please note how the lava fragments go up to what was then the glacial front in Scandinavia. There is another transatlantic band further to the south which runs up to the then-glacial front on the American side.
http://rockglacier.blogspot.com/2010/04/tephrostratigraphy.html

http://www.tephrabase.org/cgi_bin/tbase_lst1.pl?country=x




Laacher See tephra blown by winds away from point of origin in West Germany.










Lac Lautrey core indicating presence of tephra in pereiod of 14 to 8 thousand years BP. The margin for error includes the same C14 date correction used by several of the "Clovis comet" theorists.



"Bombe Volcanique" from Le Puy region, France.

http://www.colorado.edu/INSTAAR/AW2004/get_abstr.html?id=67


TOWARDS A TEPHROCHRONOLOGY FRAMEWORK FOR THE LAST GLACIAL/INTERGLACIAL TRANSITION IN SCANDINAVIA AND THE FAROE ISLANDS

WASTEGåRD, STEFAN Department of Physical Geography and Quaternary Geology, Stockholm University, Sweden.
Davies, Siwan M. Department of Geography, University of Wales Swansea, UK.
Turney, Chris S.M. School of Archaeology and Palaeoecology, Queen's University, Belfast, UK.
Wohlfarth, Barbara Department of Physical Geography and Quaternary Geology, Stockholm University, Sweden.


The Last Glacial/Interglacial transition (LGIT; ca 15-8 cal. ka BP) was a period of rapid climatic transitions around the North Atlantic. Although close similarities are evident in the palaeoclimatic reconstructions obtained from terrestrial, marine and ice-core records for the LGIT, uncertainties exist as to the degree of synchroneity (or asynchroneity) between them, largely due to the limitations of the radiocarbon dating method (radiocarbon plateaux, reservoir effects) and the lack of suitable dating methods for the time period before ca 40 ka BP. Therefore, new approaches are required for geochronology models and correlation of sequences and events. One method that holds much promise of effecting more precise regional correlations is tephrochronology.

Ten years ago, only three tephra horizons were described from this time period in Scandinavia and the Faroes: the Saksunarvatn Tephra (ca 10.2 cal. ka BP), the Vedde Ash (ca 12.0 cal. ka BP) and the Laacher See Tephra (LST, ca 12.9 cal. ka BP). The first two of these are of Icelandic origin while the LST has its origin in the Eifel volcanic field in SW Germany.

A technique for extracting cryptotephra (a tephra horizon invisible to the naked eye) has revolutionised the application of tephrochronology in minerogenic deposits from the LGIT (Turney, 1998). This technique relies upon the difference between the specific gravity of the tephra shards and the host sediment matrix and has led to the first discovery of the Vedde Ash on the British mainland as well as the previously unrecorded Borrobol Tephra, dated to ca. 14.4 cal. ka BP (Fig. 1; e.g. Turney et al., 1997). In Sweden, this technique led to the first discovery of the Vedde Ash, as well as a previously unrecorded rhyolitic tephra dated to ca 10.2 cal. ka BP (the Högstorpsmossen Tephra; Björck et al., 2002). The rhyolitic component of the Vedde Ash was also found in two sites on the Karelian Isthmus in NW Russia, greatly extending the distribution of this important marker horizon (Fig. 1; Wastegård et al., 2000). Recently, the Borrobol Tephra and two new tephra horizons, the Hässeldalen Tephra (ca 11.5 cal. ka BP) and the Askja 10-ka Tephra (ca 11.2 cal. ka BP) were discovered in LGIT deposits from Blekinge, SE Sweden, (Fig. 1; Davies et al., 2003). An effort to date the Borrobol Tephra in Sweden using wiggle-matching of AMS-dates to the Cariaco basin chronology (Hughen et al., 2004) yielded an age of ca 13.9 cal. ka BP, indicating that the Borrobol Tephra in Sweden and Scotland either represents two separate eruptions from the same volcanic system, or that the British age estimate is slightly too old (Davies et al., 2004). Lacustrine records from Andøya, north Norway (Fig. 1) extending back to ca 20 cal. ka BP are also under investigation as well as the classic Vallengaard mose site on Bornholm, Denmark (Fig. 1) that contains a visible occurrence of the Laacher See Tephra (ca 12.9 cal. ka BP).

Sediments from the Lateglacial seem to be missing on the Faroe Islands in the North Atlantic, probably due to an extensive ice cover during the Younger Dryas which may have removed older deposits. The Saksunarvatn Tephra is visible in several sections and in lake sediments and is an important marker horizon for the Early Holocene. Silicic tephra horizons below the Saksunarvatn Tephra have been found at two sites, the L3574 Tephra (Dugmore and Newton, 1998) from Lake Saksunarvatn (the type site for the Saksunarvatn Tephra) and the Hovsdalur Tephra dated to ca 10.5 cal. ka BP (Wastegård, 2002). The highly silicic Hovsdalur Tephra has an identical geochemistry to the Hässeldalen Tephra (Fig. 2), but is ca 1000 years younger. A rhyolitic tephra called the Suduroy Tephra, dated to 8 cal. ka BP was also found in the Hovsdalur site on the southern island of Suduroy. This tephra has a geochemistry similar to the rhyolitic component of the Vedde Ash and the IA2 tephra from the Rockall Trough, west of Ireland (ca 13.5-13.0 cal. ka BP; Bond et al., 2001). This indicates that “Vedde-like” rhyolitic eruptions of the Katla volcano may have persisted during the Lateglacial into the Early Holocene. After the Holmsá event (ca 7.6 cal. ka BP; Larsen, 2000) the composition of the silicic magma below the Katla volcano seems to have changed to a more dacitic composition. This is indicated by the fairly homogeneous composition of the so called SILK tephras erupted between the Holmsá and Eldgjá (AD 930s) events (Larsen et al., 2001).



REFERENCES
Björck, J., Andrén, T., Wastegård, S., Possnert, G., and Schoning, K., 2002, An event stratigraphy for the Last Glacial-Holocene transition in eastern middle Sweden: results from investigations of varved clay and terrestrial sequences. Quaternary Science Reviews v. 21, p. 1489-1501.

Bond, G., Mandeville, C., and Hoffmann, S., 2001, Were rhyolitic glasses in the Vedde ash and in the North Atlantic's Ash Zone 1 produced by the same volcanic eruption? Quaternary Science Reviews v. 20, p. 1189-1199.

Davies, S. M., Branch, N. P., Lowe, J. J., and Turney, C. S. M., 2002, Towards a European tephrochronological framework for Termination 1 and the Early Holocene. Philosophical Transactions of the Royal Society of London Series A: Mathematical, Physical and Engineering Sciences v. 360, p. 767-802.

Davies, S. M., Wastegård, S., and Wohlfarth, B., 2003, Extending the limits of the Borrobol Tephra to Scandinavia and detection of new early Holocene tephras. Quaternary Research v. 59, p. 345-352.

Davies, S. M., Wohlfarth, B., Wastegård, S., Andersson, M., Blockley, S., and Possnert, G., 2004, Were there two Borrobol Tephras during the early Late-glacial period: implications for tephrochronology? Quaternary Science Reviews v. 23, p. 581-589.

Dugmore, A. J., and Newton, A. J., 1998, Holocene Tephra Layers in the Faroe Islands. Fróðskaparrit v. 46, p. 191-204.

Hughen, K., Lehman, S., Southon, J., Overpeck, J., Marchal, O., Herring, C., and Turnbull, J., 2004, 14C Activity and Global Carbon Cycle Changes over the past 50,000 years. Science v. 303, p. 202-207.

Larsen, G., 2000, Holocene eruptions within the Katla volcanic system, south Iceland: Characteristics and environmental impact. Jökull v. 49, p. 1-28.

Larsen, G., Newton, A., Dugmore, A., and Vilmundardóttir, E., 2001, Geochemistry, dispersal, volumes and chronology of Holocene silicic tephra layers from the Katla volcanic system, Iceland. Journal of Quaternary Science v. 16, p. 119-132.

Mangerud, J., Furnes, H., and Johansen, J., 1986,. A 9000-year-old ash bed on the Faroe Islands. Quaternary Research v. 26, p. 262-265.

Mangerud, J., Lie, S. E., Furnes, H., Kristiansen, I. L., and Lømo, L., 1984, A Younger Dryas ash bed in western Norway, and its possible correlations with tephra in cores from the Norwegian Sea and the North Atlantic. Quaternary Research v. 21, p. 85-104.

Turney, C. S. M., 1998, Extraction of rhyolitic component of Vedde microtephra from minerogenic lake sediments. Journal of Paleolimnology v. 19, p. 199-206.

Turney, C. S. M., Harkness, D. D., and Lowe, J. J., 1997, The use of microtephra horizons to correlate late-glacial lake sediment successions in Scotland. Journal of Quaternary Science v. 12, p. 525-531.

Usinger, H., 1977, Bölling-Interstadial and Laacher Bimstuff in einem neuen Spätglazial-Profil aus dem Vallensgård Mose/Bornholm. Mit pollen-größenstatistischer Trennung der Birken. Geological Survey of Denmark, Yearbook, p. 5-29.

Wastegård, S., 2002, Early to Middle Holocene silicic tephra horizons from the Katla volcanic system, Iceland: new results from the Faroe Islands. Journal of Quaternary Science v. 17, p. 723-730.

Wastegård, S., Wohlfarth, B., Subetto, D. A., and Sapelko, T. V., 2000, Extending the known distribution of the Younger Dryas Vedde Ash into northwestern Russia. Journal of Quaternary Science v. 15, p. 581-586.

Figure 1. Map showing investigated sites in Sweden, Denmark (black diamonds) and the Faroe Islands. The type sites for the Vedde Ash, the Borrobol Tephra and the Saksunarvatn Tephras are also marked as well as volcanic centres on Iceland.
Figure 2. Biplot of SiO2 and K2O concentrations in tephras from the LGIT in Scandinavia and the Faroe Islands. The envelopes show the composition in tephra from some of the main European volcanic provinces (modified after Mangerud et al., 1984 and Davies et al., 2002).

Figure 3. Table 1. Tephra horizons from the LGIT (ca 15-8 cal. ka BP) found in terrestrial deposits in Scandinavia and the Faroe Islands. Ages are given as cal yr. BP This does seem to indicate a continuing series of eruptions starting at the Youngest Dryas event ("Clovis Comet" C14 corrected date of 12-13 thousand BC but direct C14 date of 10-11 thousand BP on average) and continuing on as an aftershock to approx. 6000 BC [which is about the time of the Mt. Mazama ash (Crater lake formation), an eruption of Mt. St. Helens and major eruptions also in Kamchitka, Siberia and in Japan.] I would count the ash deposits from ALL the events between Laacher See to Hogstorpsmossen (12000 to 10200 years ago by the chart) as probably about the same date within a margin for error and as levels representing the same event or related events. Some of the ash got as far as Spitzbergeb, by the way.

The important thing to realise is that basically the entire floor of the North Atlantic is covered with fragments of aerated lava at about this same date, and large areas of Europe and probably North Africa, Mexico and the Caribbean are also. It is a known fact that there were major eruptions going on in the Azores and Canary Islands as well as Iceland, simultaneously, and then a large number of "Ring of Fire" volcanoes erupting at a slightly later, delayed date, with some of the echo-eruptions going on for as many as two or three thousand years afterwards.

Best Wishes, Dale D.

1 comment:

  1. After publishing the article it occurs to me that not only is the volcanic bomb from the Azores evidence of widespread eruptions at the time, so is the soil it is shown resting on. It is decomposed volcanic ash of probably the same age and it is much like the loess you see in North America, Europe and Asia. Some experts have considered the chemical composition of loess to be like volcanic ash and Muck believes that is the true origin on loess. In the Midwest and Mississippi valley areas, the true loess is the peoria loess and it C14 dates to the same general horizon as given to the other volcanic ejecta here: 10 to 12 thousand years old on average by direct radiocarbon date, somewhat older when assuming an additional correctional factor.

    Best Wishes, Dale D.

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