.mw-parser-output .hidden-begin{box-sizing:border-box;width:100%;padding:5px;border:none;font-size:95%}.mw-parser-output .hidden-title{font-weight:bold;line-height:1.6;text-align:left}.mw-parser-output .hidden-content{text-align:left}@media all and (max-width:500px){.mw-parser-output .hidden-begin{width:auto!important;clear:none!important;float:none!important))You can help expand this article with text translated from the corresponding article in German. (January 2009) Click [show] for important translation instructions. View a machine-translated version of the German article. Machine translation, like DeepL or Google Translate, is a useful starting point for translations, but translators must revise errors as necessary and confirm that the translation is accurate, rather than simply copy-pasting machine-translated text into the English Wikipedia. Consider adding a topic to this template: there are already 9,120 articles in the main category, and specifying|topic= will aid in categorization. Do not translate text that appears unreliable or low-quality. If possible, verify the text with references provided in the foreign-language article. You must provide copyright attribution in the edit summary accompanying your translation by providing an interlanguage link to the source of your translation. A model attribution edit summary is Content in this edit is translated from the existing German Wikipedia article at [[:de:Naturpark Niederlausitzer Heidelandschaft]]; see its history for attribution. You may also add the template ((Translated|de|Naturpark Niederlausitzer Heidelandschaft)) to the talk page. For more guidance, see Wikipedia:Translation.
Watermill in Plessa
Watermill in Plessa

The Lower Lusatian Heath Nature Park (German: Naturpark Niederlausitzer Heidelandschaft) is a nature park and reserve in the state of Brandenburg, Germany. It covers an area of 490 km2 (189 sq mi). It was established on May 24, 1996.

In the south, where Brandenburg's oldest landscape is found, the area was formed approximately 180,000 years ago at the end of the ice age, with its glacial valley. Among the ice-age deposits are massive coal layers. After extensive mining in the last hundred years, the landscapes has developed a unique and in some parts, a bizarre appearance. In many places are valuable specialized habitats for animals and plants.

51°30′56″N 13°23′39″E / 51.5156055556°N 13.3940388889°E / 51.5156055556; 13.3940388889