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T<\/span>he low\u00ader Oder Val\u00adley is one of the last near-nat\u00adur\u00adal riv\u00ader flood\u00adplain land\u00adscapes in Cen\u00adtral Europe, vast\u00adly unde\u00advel\u00adoped and some\u00adtimes wild and harsh beau\u00adty. Over a length of 60 kilo\u00adme\u00adters and an aver\u00adage width of 3 kilo\u00adme\u00adters, i.e. in a rel\u00ada\u00adtive\u00adly lim\u00adit\u00aded space, it com\u00adbines an abun\u00addance of very dif\u00adfer\u00adent habi\u00adtat types. On the one hand there are the aquat\u00adic habi\u00adtats, where\u00adby a dis\u00adtinc\u00adtion must be made between the riv\u00ader or on the east\u00adern edge of the val\u00adley and the Hohen\u00adsaat\u00aden-Friedrich\u00adsthaler water\u00adway on the west\u00adern edge of the val\u00adley, in between the many inter\u00adcon\u00adnect\u00aded back\u00adwa\u00adters in the flood\u00adplain itself.<\/p>\nSev\u00ader\u00adal crys\u00adtal clear spring brooks arise from the slopes of the Oder val\u00adley, and there are also some larg\u00ader rivers such as the Welse or Salvey\u00adbach on the west and the R\u00f6hrike (Rurzy\u00adca) on the east. In the flood\u00adplain itself, the exten\u00adsive sedge, reed and reed stands are par\u00adtic\u00adu\u00adlar\u00adly dis\u00adtinc\u00adtive, but so is the hard\u00adwood and soft\u00adwood allu\u00advial for\u00adest, at least in rem\u00adnants. On the val\u00adley slopes, the lat\u00ader\u00adal moraines of the Oder val\u00adley, which was formed as a glacial val\u00adley in the post-ice age, there are species-rich, nat\u00adur\u00adal decid\u00adu\u00adous forests, and flow\u00adery dry grass on the heights.<\/p>\n<\/div><\/div><\/i><\/span>For\u00adest<\/a><\/div><\/li><\/i><\/span>Xeric grass\u00adlands<\/a><\/div><\/li><\/i><\/span>Pold\u00aders<\/a><\/div><\/li><\/i><\/span>Back\u00adwa\u00adter, oxbow lakes, pools<\/a><\/div><\/li><\/ul><\/div><\/div><\/div>\n\t\t
Sev\u00ader\u00adal crys\u00adtal clear spring brooks arise from the slopes of the Oder val\u00adley, and there are also some larg\u00ader rivers such as the Welse or Salvey\u00adbach on the west and the R\u00f6hrike (Rurzy\u00adca) on the east. In the flood\u00adplain itself, the exten\u00adsive sedge, reed and reed stands are par\u00adtic\u00adu\u00adlar\u00adly dis\u00adtinc\u00adtive, but so is the hard\u00adwood and soft\u00adwood allu\u00advial for\u00adest, at least in rem\u00adnants. On the val\u00adley slopes, the lat\u00ader\u00adal moraines of the Oder val\u00adley, which was formed as a glacial val\u00adley in the post-ice age, there are species-rich, nat\u00adur\u00adal decid\u00adu\u00adous forests, and flow\u00adery dry grass on the heights.<\/p>\n<\/div>