Hille is located in the northeast of the
Detmold (region), in the middle of the
Minden Land. Hille has portions of the ecologic areas of the
Wiehen Hills, the Lübbecke Loess Country and the Rahden-Diepenauer Sandy Moorlands (boglands). The southern portion of the community is located in the transition zone from the North Germain Plain to the
Central Uplands (piedmont). This especially apparent with the ridgelike structure of the Wiehengebirge, which closes Hille like a bolt from the
Ravensberg hill country. The main part of the northerly bench of the community is clearly a component of the plain, which received its end
moraine character from the Ice Age. The Great Peatbog (
Grosses Torfmoor) provides Hille with a wet ecosystem of glacial origin which has been a designated nature reserve since 1980. This is where rare plants and animals such as white storks are found. Hille is the source of the Ösper, a tributary of the River
Weser. The
Mittelland Canal crosses Hille at its geographic middle in an east–west orientation. Several settlements adhere to the canal's adjacent dry northern plateau. To the north are a large
raised bog and the Minden Forest (
Mindener Wald). The River Weser presents a geographic border 10 km east of Hille. To the west the same landscape continues all the way to Osnabrück. The varied farmland is characterized by scattered settlements and single farms that are bordered by copses and hedges. Forests are found on higher ground, while meadows are found at low ground and in bogs.
Neighbouring municipalities •
Petershagen •
Minden •
Bad Oeynhausen •
Hüllhorst •
Lübbecke •
Espelkamp •
Uchte in
Lower Saxony Subdivisions of the municipality After the local government reforms of 1973, Hille consists of 9 districts: • Hille-Dorf • Hartum • Nordhemmern • Holzhausen II • Südhemmern • Eickhorst • Rothenuffeln • Oberlübbe • Unterlübbe
Geology The community land formation was primary influenced by the Saalian Stage (Wolstonian Stage and Illinoian Stage are Equivalents) ice age, as well as pre and post glacial process. At the time the area was covered with ice, the flow of water had an opposite direction to that of the present, that is it flowed from the ice to the south, collected in a riverine environment north of the Wiehengebirge and flowed to the west to reach the sea. Extensive wet bogs were created in this historic river valley, that remained impassable for humans for a long time. Remains of this exist in the Great Peat Bog (Große Torfmoor) that is now a protected nature preserve.
Soils The mentioned glacial conditions created various fertilities of soil, with varying impact on the structure of settlement. As a result, there is fertile soil in the south between the Wiehengebirge and the
Bastau lowland, which is referred to as Lübbecke
Loessland. Besides the settlement of Rothenuffeln, the villages of Oberlübbe, Unterlübbe and Eickhorst developed here. The Bastau lowland connects to the north, in which there can be no significant agriculture. Because of this the Mittellandkanal is located at its northern edge. The Hartume loess plate lies to the Northeast of the Bastau lowland, where there are good opportunities for agriculture. The villages of Hartum, Nordhemmern, Südhemmern and Holzhausen II are located here. The farmsteads are of middling size with 100 morgen(1 morgen = 3 acres) not being uncommon. This loess plate continues to the westward beyond the stream Flöthe, where the village of Hille is the center of settlement. The northeast of the community of Hille has poor soil that allows only forestry( Mindener Wald) to exist.
Fauna The
white stork nests in and around the Bastau lowland, with assistance provided for its recovering population.
Extent and utilization of the Community Area Hille is classified as a "large rural community" that lies in the
North German Plain, it rises to the ridge of the Wiehengebirge in the south. The Lübber Berg (mountain) is its highest point at an altitude of 251m over sea level. The lowest point is in the Bastau lowland meadows or bogs near Hartum with an altitude of only 47.7m. Hille extends 11.8 km from east to west and 15.4 km from north to south. ==History==