The highest point of the Löwenstein Hills, at 561.0 m, is the wooded Raitelberg west of Wüstenrot; roughly north of this "hill" is the Stangenberg. The forested Horkenberg between Löwenstein and Wüstenrot, at 549.0 m, is very high. The Stocksberg which belongs to Beilstein and Löwenstein and the Juxkopf near Spiegelberg with its Juxkopf Tower have good views. To the west in the Heilbronn forest area of the Heilbronn Hills is the Schweinsberg and another observation tower, the Schweinsberg Tower, the Heilbronn Transmission Tower and the Schweinsberg Water Tower owned by the Lake Constance water company, Bodensee-Wasserversorgung. To the south where the hills transition into the Mainhardt Forest, the wooded Black Jurassickuppen between the Lauter valley and Fischbach valley heights rise up to 565.7 m.
Rivers and streams
The following rivers and larger streams drain the Lowenstein Hills or are catchment waters on its perimeter.
The Murr rises not far from Murrhardt in the Murrhardt Forest, flows mainly westwards via Murrhardt and Backnang to Marbach, where it empties into the Neckar. Part of its course flows through the southeast of the Löwenstein Hills.
* The Lauter rises near Löwenstein-Hirrweiler, flows southeastwards through Spiegelberg and discharges near Sulzbach into the Murr.
* The Klöpferbach rises north of Rietenau, flows south through Aspach and joins the Murr near Backnang-Unterschöntal.
* The Wüstenbach rises near Kleinaspach, flows mainly southwards and empties into the Murr between Burgstetten-Burgstall and Backnang.
* The Bottwar rises near Prevorst, flows southwestwards via Großbottwar to Steinheim on the Murr, where it ends.
The Schozach rises near Löwenstein, flows initially southwestwards through Abstatt to Ilsfeld and then northwestwards via Talheim to Heilbronn-Sontheim, where it discharges into the Neckar.
The Sulm rises near Löwenstein, flows northwestwards through the Weinsberg valley and empties near Neckarsulm into the Neckar.
Geology
Geologically the Löwenstein Hills belong to the Germanic Trias supergroup of the earth's Triassic period and are counted as part of the Keuper, which means they were formed about 220 million years ago. The highest points are isolated Black Jurassic domed summits or kuppen, which lie on the Knollenmergel. In the Löwenstein Hills there are numerous outcrops, rock formations and mining galleries, some of which have educational paths offering information about them:
Obersulm-Eichelberg, the Kolbensteige: an outcrop with rocks ranging from the Lower Bunter Marl to the Lowest Stuben sandstone on the bank of a sunken road
Spiegelberg-Vorderbüchelberg, the Bodenbach Gorge: an erosion gorge of Stuben sandstone with a 30-metre-wide rock shelter, the Hohler Stein, and a small waterfall
Spiegelberg-Jux, the Hüttenwald Gorge: an erosion gorge, Upper Bunter Marl and Stuben sandstone
Spiegelberg-Jux, the Wetzsteinstollen, a mining gallery in the gravel sandstone, worked until 1923, in the valley of the Winterlauter
Spiegelberg-Nassach: Mining educational path in the valley of the Winterlauter with evidence of the mining of coal, construction rock, sand pits for glassmaking and the Wetzstein gallery.
Untergruppenbach: south of the motorway junction, a marl pit in the Lower Bunter Estherian beds of the gypsum keuper
Untergruppenbach-Unterheinriet: sunken road and quarry on the southern Hohberg in the reed sandstone
Wüstenrot, Pfaffenklinge: erosion gorge in the Stuben sandstone and Knollenmergel with two galleries from the 18th century, in which only pyrites was found instead of the hoped-for silver.
Literature
Thomas Huth und Baldur Junker: Geotouristische Karte von Baden-Württemberg 1:200 000 NORD. Erläuterungen.Regierungspräsidium Freiburg, Landesamt für Geologie, Rohstoffe und Bergbau, Freiburg i. Br. 2005.