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The Netherlands Environmental Assessment Agency published a map of surface water bodies in the Netherlands in 2010. [1] The map distinguishes over 20 different types of water bodies, including those with salty, brackish and fresh water. These water bodies encompass natural and artificial lakes of varying sizes, peat puddles and fens.
A series of devastating storm surges, more or less starting with the First All Saints' flood (Allerheiligenvloed) in 1170 washed away a large area of peat marshes, enlarging the Wadden Sea and connecting the previously existing Lake Almere in the middle of the country to the North Sea, thereby creating the Zuiderzee.
A lump of peat Peat stacks in Südmoslesfehn (district of Oldenburg, Germany) in 2013 Peat gatherers at Westhay, Somerset Levels in 1905 Peat extraction in East Frisia, Germany. Peat is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs.
The Lime Hollow Center for Environment and Culture (Lime Hollow) is a nature preserve project in Cortland County, New York.It was founded in 1993 as the Lime Hollow Nature Center, the culmination of efforts 20 years earlier to develop a nature preserve to protect an unusual assemblage of marl ponds, a peat bog, and kame-and-kettle topography along an abandoned railroad right of way in Lime ...
The recent Netherlands is formed by Pleistocene and Holocene age sediments as result of -fluvial, eolian and marine sedimentation. Eolian dunes characterise the North Sea coast, a horseshoe-shaped moraine forms the Utrecht Hill Ridge (Dutch: Utrechtse Heuvelrug) and the river influence is still visible all over the Netherlands.
A new element in the design of this polder was the intention to establish a larger city to serve as a regional centre for all the polders and perhaps the capital of a potential new province. This city, located in the centre of the reclaimed lands, was developed as Lelystad (1966), named after the man who had played a crucial role in the design ...
Cross Lake has a maximum depth of 65 feet and has an average depth of 18 feet. The Seneca River flows west to east through the south end of the lake. Since Cross Lake is part of the New York State Canal System, there are a variety of fish that pass through it. Cross Lake has a flushing rate of 51 times per year; once per week.
Alcove Reservoir; Allegheny Reservoir; Amawalk Reservoir; Ashokan Reservoir; Basic Creek Reservoir; Beacon Reservoir, Dutchess County; Beacon Reservoir, Putnam County; Blake Falls Reservoir