Walton Moss, Cumbria, England

Your search has found 2 tephra layers at Walton Moss

Site Type Area Latitude LongitudeGrid reference Altitude (m)
Terrestrial England, Cumbria 54.9952°N 2.7671°W NY 5102 6700 100

 

*Note that the Tephra layer depth of a cryptotephra does not indicate the thickness of the layer, as in a visible tephra tephra layer. The thickness indicates the spread of the tephra shards in the sediment or sometimes the top and bottom depths are the same (i.e. no apparent thickness).
1Correlated tephra name means that the tephra deposit has been correlated with a tephra horizon found at multiple sites (e.g. Hekla 4). Of course, these correlations could be reinterpreted and care needs to be taken.
2Local tephra name is the name given by the researchers for the tephra found at the site, this is often a mixture of a site code/name and the depth of the tephra. Not all tephra layers in Tephrabase have a local name, but more or being added. This is independent of any correlations to other tephra deposits.
Profile Tephra Layer
No Name Profile Depth (m) Type Correlated name1 Local name2 Tephra Depth (m) Comments Geochemical data Ref
1113 WLM17 10.00 Wide diameter Russian corer
Glen Garry Tephra 2.120 - 2.130 *Cryptotephra View Data 2261
1121 WLM24 10.00 Wide diameter Russian corer
Glen Garry Tephra 2.120 - 2.130 *Cryptotephra View Data 2261

References

The data on this page is from the following source(s). If you use this data please acknowledge the source of the data. The number preceding each reference matches the Ref number on the data table above.

2261: Barber, K., Langdon, P. and Blundell, A.  2008  Dating the Glen Garry tephra: a widespread late-Holocene marker horizon in the peatlands of northern Britain. Holocene  18, 31-43.

Data Sources

All of the data contained in this database is either published or donated. When using the data, acknowledgement must be made of the original source of the data and that the data was obtained from Tephrabase. See Copyright information.

This Tephrabase search was made on 4/7/2025 at 21:06:02 local time, Edinburgh, Scotland, UK.