0000000000302153

AUTHOR

Juris Soms

Seismites resulting from high-frequency, high-magnitude earthquakes in Latvia caused by Late Glacial glacio-isostatic uplift

Abstract Geologically extremely rapid changes in altitude by glacial rebound of the Earth crust after retreat of the Scandinavian Ice Sheet at the end of the last Weichselian glaciation influenced the palaeogeography of northern Europe. The uplift of the Earth crust apparently was not gradual, but shock-wise, as the uplift was accompanied by frequent, high-magnitude earthquakes. This can be deduced from strongly deformed layers which are interpreted as seismites. Such seismites have been described from several countries around the Baltic Sea, including Sweden, Germany and Poland. Now similarly deformed layers that must also be interpreted as seismites, have been discovered also in Latvia, a…

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A geomorphological approach for enhancing environmental management and conservation of landforms as protected nature objects in the Upper Daugava spillway valley

<p class="R-AbstractKeywords"><span lang="EN-GB">This paper describes the application of geomorphological approach for environmental management and conservation of landforms. Specifically, we discuss the contribution of geomorphological field survey and adapted matrix methodology (in combination with understanding of geology) to identification, study and evaluation of those abiotic nature elements which represent geological and geomorphological heritage. We describe a case study carried out in that part of the protected landscape area “Augšdaugava” which encompasses the Upper Daugava spillway valley. The study programme reported in this paper was realized to perform inventory of…

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Gravu morfoloģija, to veidošanās un erozijas tīkla izvietojuma likumsakarības dienvidaustrumu Latvijā

Elektroniskā versija nesatur pielikumus

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STOP 11: Recessional moraine ridge at Veresovka, Rāzna glacial depression

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STOP 10: Kame terrace in the Upper Daugava depression at Rakuti, near Krāslava

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STOP 13: Inland dune field near Daugavpils, East-Latvian Lowland

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STOP 9: Upper Daugava spillway valley and associated gully network at Vasargelišķi

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