Research group Stockholm University Quaternary Tephra Studies (SUQuaTeSt)

Volcanic ashes (tephra) buried in sediments or glacier ice are a useful material for geochronological applications. At Stockholm University, tephrochronology has been used in geological research over the course of the last few decades.

Tephra is the unconsolidated pyroclastic material ejected into the atmosphere during an explosive volcanic eruption. To put it in simple terms: it's the stuff that shoots up when a volcano goes "boom". The finest particles of this is the volcanic ash, and it can spread far by wind in a short amount of time. Most of it settles on the surfaces of the Earth within a few weeks at the most, which in geological terms is very quick.

Tephra that has become properly buried in sediments or glacier ice therefore becomes a very precise time-marker for the eruption event. This works as a dating method in climate reconstructions and as a correlation tool between studies where the same tephra has been identified at different locations. Tephrochronology is the method where volcanic ashes are used for chronological applications, and it is useful in various disciplines of geology, palaeontology and archaeology.

The tephra studies performed at Stockholms University today were initiated by professor Stefan Wastegård around the turn of the millenium, but its roots go further back. The term "tephra" as used to describe volcanic ashes in geology and "tephrochronology" for the chronological applications of volcanic ashes were coined by Sigurdur Thorarinsson in 1944, in his disseration at Stockholms högskola (Stockholm University College). The more recent research has involved several PhD students and postdocs as well as collaborators from other institutions.

The field equipment and laboratory facilities at the Department of Physical Geography allow for field sampling and laboratory extraction of tephra in sediments. Detection of ash particles is performed via microscopy, while adequate geochemical analysis requires equipment currently not hosted at Stockholm University. The recent and current research mainly has a Quaternary geology and palaeoclimate focus, but methodological and other aspects of tephra studies and their advancement are also of interest.

This research group has no members.

There are no research project connections.

Larsen, E., et al. (2025) Volcanically induced glacier collapses in southern Jan Mayen (Sør-Jan), Norway. https://doi.org/10.1111/bor.12687

Larsson, S.A., (2025) From the ashes: a 150th anniversary review of the Askja-1875 tephra. https://doi.org/10.58051/ns01-jf70

Moore, C.R., et al. (2026) Stratigraphic Separation of Laacher See Tephra and a Discrete Younger Dryas Boundary Fallout Layer in Southernmost Sweden [preprint]. https://doi.org/10.14293/PR2199.003441.v1

Recommendations for using XRF core scanning as a tool in tephrochronology - Recommendations for using XRF core scanning as a tool in tephrochronology

Tephra horizons contemporary with short early Holocene climate fluctuations: New results from the Fa - Tephra horizons contemporary with short early Holocene climate fluctuations: New results from the Faroe Islands

A Lateglacial–early Holocene tephrochronology for SW Sweden - A Lateglacial–early Holocene tephrochronology for SW Sweden

A Late Younger Dryas–Early Holocene tephrostratigraphy for Fosen, Central Norway - A Late Younger Dryas–Early Holocene tephrostratigraphy for Fosen, Central Norway

Faroe Marine Ash Zone IV: a new MIS 3 ash zone on the Faroe Islands margin - Faroe Marine Ash Zone IV: a new MIS 3 ash zone on the Faroe Islands margin

Lateglacial cryptotephra detected within clay varves in Östergötland, south-east Sweden - Lateglacial cryptotephra detected within clay varves in Östergötland, south-east Sweden

Compositions of glass in proximal tephras from eruptions in the Azores archipelago and their links w - Compositions of glass in proximal tephras from eruptions in the Azores archipelago and their links with distal sites in Ireland

Revisiting the Borrobol Tephra - Revisiting the Borrobol Tephra

The Laacher See Tephra discovered in southernmost Sweden - The Laacher See Tephra discovered in southernmost Sweden

Towards a Holocene tephrochronology for the Faroe Islands, North Atlantic - Towards a Holocene tephrochronology for the Faroe Islands, North Atlantic

Rhyolitic and dacitic component of the Askja 1875 tephra in southern and central Finland: first step - Rhyolitic and dacitic component of the Askja 1875 tephra in southern and central Finland: first step towards a Finnish tephrochronology

New major element analyses of proximal tephras from the Azores and suggested correlations with crypt - New major element analyses of proximal tephras from the Azores and suggested correlations with cryptotephras in North-West Europe

Hekla 1947, 1845, 1510 and 1158 tephra in Finland: challenges of tracing tephra from moderate erupti - Hekla 1947, 1845, 1510 and 1158 tephra in Finland: challenges of tracing tephra from moderate erupti

Palaeolake sediment records reveal a mid- to late Younger Dryas ice-sheet maximum in Mid-Norway - Palaeolake sediment records reveal a mid- to late Younger Dryas ice-sheet maximum in Mid-Norway

A high-resolution Lateglacial–Early Holocene tephrostratigraphy from southernmost Sweden with commen - A high-resolution Lateglacial–Early Holocene tephrostratigraphy from southernmost Sweden with commen

Synchronous or Not? The Timing of the Younger Dryas and Greenland Stadial-1 Reviewed Using Tephrochr - Synchronous or Not? The Timing of the Younger Dryas and Greenland Stadial-1 Reviewed Using Tephrochr

A Holocene tephrochronological framework for Finland - A Holocene tephrochronological framework for Finland