1974BoreasRequires access

Younger Dryas end moraines between Hardangerfjorden and Sognefjorden, Western Norway

Inge Aarseth, Jan Mangerud

Open publisher page 75 citations

Abstract

End moraines (called the Herdla Moraines) from the Younger Dryas Stadial arc morphologically mapped along the western coast of Norway, from Hardangerfjorden to north of Sognefjorden. The submarine position of the moraines are found by means of a conventional echo sounder. Stratigraphieal studies with many C14 datings are used for age determination, giving Late Younger Dryas (10,000–10,500 C14 years B.P.) for the Herdla Moraines. The moraines are correlated with the Ra‐Salpausselkä Moraines. Isobases for the Younger Dryas are obtained from marine terraces formed contemporaneously with the moraines.

About this research paper

What this paper is about

End moraines (called the Herdla Moraines) from the Younger Dryas Stadial arc morphologically mapped along the western coast of Norway, from Hardangerfjorden to north of Sognefjorden. The submarine position of the moraines are found by means of a conventional echo sounder. Stratigraphieal studies with many C14 datings are used for age determination, giving Late Younger Dryas (10,000–10,500 C14 years B.P.) for the Herdla Moraines. The moraines are correlated with the Ra‐Salpausselkä Moraines. Isobases for the Younger Dryas are obtained from marine terraces formed contemporaneously with the moraines.

Why it matters

OpenAlex reports 75 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

End moraines (called the Herdla Moraines) from the Younger Dryas Stadial arc morphologically mapped along the western coast of Norway, from Hardangerfjorden to north of Sognefjorden. The submarine position of the moraines are found by means of a conventional echo sounder. Stratigraphieal studies with many C14 datings are used for age determination, giving Late Younger Dryas (10,000–10,500 C14 years B.P.) for the Herdla Moraines. The moraines are correlated with the Ra‐Salpausselkä Moraines. Isobases for the Younger Dryas are obtained from marine terraces formed contemporaneously with the moraines.

Key concepts: Younger Dryas, Moraine, Geology, Allerød oscillation, Stadial, Terminal moraine, Glacial period, Physical geography

Related papers

Back to paper searchBrowse research topicsOriginal source
Younger Dryas end moraines between Hardangerfjorden and Sognefjorden, Western Norway — Research Paper | ScholarLens