description Šeškinė Esker Overview
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Šeškinė Esker ranks #22 of 148 in the Esker ranking, behind Pytkynharju, ahead of Hiittenharju.
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How was the Šeškinė Esker formed?
The ridge was built from sand and gravel deposited by meltwater flowing within or beneath glacial ice. When the ice retreated after the last glacial period, the stream deposit remained as a long, narrow landform called an esker.
Where is the Šeškinė Esker in Vilnius?
It lies in the Šeškinė area of Lithuania's capital, embedded within a modern urban district. Its survival gives visitors a visible piece of glacial geology without leaving Vilnius.
Why is the Šeškinė Esker protected?
It is protected as a geological monument because urban development has erased or altered many comparable glacial features. The ridge preserves evidence of how meltwater moved through the ice that once covered the Vilnius region.
Is the Šeškinė Esker a man-made embankment?
No. Its narrow raised shape can resemble a road or railway embankment, but it is a natural deposit left by a subglacial stream during the last ice age.
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