|Basin countries||United Kingdom|
The Mere lies within the borough of Stafford in Staffordshire, England, some 3 km east of the market town of Newport, Shropshire. It is within the grounds of Aqualate Hall, a country house, with a landscaped deer park.
Although large in extent (1.5 km long and 0.5 km wide), the Mere is remarkably shallow and is nowhere much more than one metre deep. Aqualate Mere is an example of an esker system (rare in the Midlands) formed by glacial meltwaters during the late Devensian glaciation, about 50,000 years ago. The depression in which the Mere lies, thought to be a kettle hole, and the surrounding higher ground which comprises glacial sand and gravel deposits were all formed at the same time.
The Mere supports diverse fish and bird populations, including large numbers of wintering and breeding wildfowl and breeding Eurasian curlew and common snipe. Together with the surrounding land, it is also important for its botanical and invertebrate communities. Mammals found on the NNR include polecat, water vole and harvest mouse, together with bats such as pipistrelle, Daubenton's, Natterer's, Brandt's and whiskered.
Its name came from Anglo-Saxon Āc-gelād = "oak grove".
- "Aqualate Mere National Nature Reserve (NE405)". Natural England. 1 March 2013. Retrieved 3 January 2016.
- Staffordshire Regionally Important Geological and Geomorphological Sites Group - Aqualate Mere Archived July 21, 2011, at the Wayback Machine.
- An integrated lake-catchment approach to reconstruct land use changes and pollution history at Aqualate Mere, Central England, UK. Retrieved 2016-01-03.
- John Shipley The Little Book of Shropshire- 2015 0750963425 "The site chosen was a sandstone ridge to the west of Aqualate Mere, a natural lake, the largest in the Midlands, formed by melting glaciers; the River Meese flows from here to the River Tern. The lake and its abundant fisheries are mentioned .."
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