Tadcaster - Conservation

Conservation

To the south east of the town centre, towards the village of Oxton, lies Tadcaster Mere. Designated as a Site of Special Scientific Interest or SSSI in 1987, the Mere is in fact the central part of a former lake basin which extended over an area of about 3 kmĀ². It was formed during the most recent or Devensian ice age (which ended 10,000 years ago, when present-day Tadcaster would have been situated at the southernmost limit of glaciation) by the long, low embankment of debris known as the Escrick Moraine, which is composed of debris left behind by the Vale of York Glacier. The Mere is a site of current palaeontological interest, as it is currently believed to be the site of the earliest discovery of the plesiosaur (while unproven, the skeletal fragments found in Tadcaster at the least match the age of those found elsewhere).

Scientific analysis of the mere, in particular sedimentary pollen studies, provides insight into the geological history and makeup of the local environment and allows accurate dating of events before, during and after the Devensian ice age.

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Famous quotes containing the word conservation:

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