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The seasonal wetland of Peräkorpi changes during the year. In springtime it's a beautiful pond, but in summertime it dries to a mossy and grassy meadow. In the autumn it starts collecting water again, and in the wintertime it is covered by ice. The seasonal variation is caused by porous and sandy soil. The water in the pond just seeps into the ground and turns into groundwater. Even though the vegetation in the wetland is typical mire vegetation, it does not form any peat.

Nearby attractions: Annelid traces in sandstone, The tor formations of Aumakalliot, Aumakivi tor corestone, The Kivijata of Huhtakorpi, Kaivolammi lake, Springtime in Peräkorpi, The southern end of Kivijata boulder field, Kivijata stone field, Kivijata then and now, The highest post-glacial shoreline, The Lauhankangas highest shoreline, Old sandstone mining pits of Korsukangas, The boulder field of Korsukankaan kivijata, Kuivajärvi - a lake that disappears, The day trip hut of Kärkikeidas, Lauhanvuori National Park, The observation tower of Lauhanvuori, Lauhanvuori-Hämeenkangas Geopark, The lean-to shelter of Leikkistenkangas, Wild Forest Reindeer camera, Duckboard trail on the Peräkorpi spruce mire, Lake Spitaalijärvi

Coordinates (WGS84): 62.13841, 22.15009

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Keywords: 360-image, Geosite, Groundwater, Mire, Pond