English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

The Sami word ráhppát means rough bouldery/stony terrainwith sharp-relief topography in Finnmark, northern Norway.Ráhppát is a common name in the region of the Younger Dryaslandforms, yet the origin of ráhppát has remained obscure.The timing of the Younger Dryas is concomitant with the maximum neotectonicfault instability in Fennoscandia. Hence, earthquake activity may have beenone of the contributing factors for the Younger Dryas morphologies.Ráhppát on the Maskevarri fell, classified as a part ofTromsø-Lyngen sub-stage of the Younger Dryas, was studied by means ofgeomorphology and measurements of electrical-sedimentary anisotropy.Ráhppát was found to be built up of an anastomosing networkof stony esker-like ridges and mounds bordered with arch-shaped andsinusoidal ridges. These bordering ridges exhibit sedimentary (azimuthal soilelectrical conductivity) anisotropy parallel-to-ridge trends and wereinterconnected to meltwater gullies suggesting generation through short-livedconduit infills. We did not find electrical-sedimentary evidence to supportthe concept of englacial thrusting and/or compression, often described forYounger Dryas moraines. Maskevarri Ráhppát is typified by ~ 500ponds and small lakes on three different elevations descending in an up-icedirection. These may have generated through late glacial earthquake(s) alsocontributing to subglacial deformation of Maskevarri Ráhppát

Maskevarri Ráhppát in Finnmark, northern Norway – is it an earthquake-induced landform complex?