Concretions in glacial sediments at Seglvatnet, Norway.

Research output: Contribution to journalArticlepeer-review


Concretions in Pleistocene glacial sediments at Seglvatnet, Norway, include a wide variety of forms, the simplest of which apparently reflects relatively uniform growth rates in different directions; the preferred orientation of others may be associated with water movement through the sediments. Concretion shape generally is influenced by the grain size and bedding of the enveloping sediments. Some concretions may have formed during, or soon after, deposition of the sediments; others are forming at present. -Author
Original languageEnglish
Pages (from-to)191-196
Number of pages5
JournalJournal of Sedimentary Petrology
Issue number1
Publication statusPublished - 1981


Dive into the research topics of 'Concretions in glacial sediments at Seglvatnet, Norway.'. Together they form a unique fingerprint.

Cite this