Vilnius
Šeškinės ozas
개요
Šeškinės ozas atsirado prieš 16-18 tūkst. metų, paskutinio pleistoceno ledyno pakraštyje, kur ledas užėmė pažemėjimą. Ozas susidarė iš fliuvioglacialinių sąnašų stambiame ledo plyšyje. Visai ištirpus ledynui ir šioms sąnašoms suslūgus, žemės paviršiuje išryškėjo pailgas vingiuotas kalvagūbris, kurio dabar matoma tik viršutinė dalis.
Šeškinės Oz appeared before the 16-18 thousand. years, the last Pleistocene glacier edge, where the ice had drop in. Oz fluvic deposits formed from a major ice slot.
When glacier has melted and the following drift shrunken on the ground surface showed elongated sinuous ridge, which is now seen only in the upper part.
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