Geologically considered, the Hohenlohe-level is part of the southwest German Schichtstufenlandes (cuesta country) and belongs to the Triassic landscape.
It is one of a band with varying breadth from the south-eastern edge of the Black Forest on the Franconian Gäubucht up to Franconia in the north extending to Gäuflächen and passes north and east into the Bauland region, the Tauber Valley, and the Haller Plain.
The Hohenlohe plane itself includes the area around the Kocher river and Jagst river, to the foot of the mountains and Keuper forest, and is a forest-poor and fertile old farmland.

In the subsurface are the layers of the Muschelkalk period, on the wide open spaces of layers of the Lower Keuper and are partially covered by loam.
The most hard rock of the Muschelkalk in Tauber, Kocher, and its many tributaries of the Jagst river have cut and made it close, varied and scenic valley portions.
The Gäufläche is framed in the southern semicircle of the forests of the Löwenstein, Waldburger Limpurger and mountains and dominates it.[7]
This Keuper perimeter dominates the Hohenlohe level by about 130 metres (430 ft), in Waldenburg even up to 180 metres (590 ft).
The Stufenbildner is mainly on reeds, gravel and sandstone, because of waterlogging little, but are mainly forested.
By fluvial erosion of the edge of the Keuper forest mountains over time has been divided into several sections with spur-like projections.
In some places individual mountains were separated, at Öhringen: the Golberg (325 metres, 1,066 ft), the Verrenberg (205 m) and the Lindelberg (334 metres, 1,096 ft).
The landscape around Öhringen shares two important elements of the Southwest German cuesta country: the Gäuplatten and the Keuper forest mountains.

The limestone in the subsurface of Hohenlohe and Haller is widely karstified, as evidenced by more than 2,000 sinkholes, many dry valleys and a few cave systems.
In several limestone quarries, the rock is mined and usually broken into gravel, even in the town of Öhringen (at Unterohrn).
However, the limestone deposited in a little water-permeable layer nor Lower Keuper, which prevents a rapid infiltration of precipitation in the limestone.
Moreover, as the Lower Keuper often has loess, this has created mineral-rich, arable soil easy to work with sufficient moisture.

The area surrounding Öhringen is strongly influenced by agriculture.
Besides the cultivation of cereals, sugar beet, cabbage, corn, and rapeseed, the orchards and vineyards give the landscape for mi around its typical character.
Geologically considered, the Hohenlohe-level is part of the southwest German Schichtstufenlandes (cuesta country) and belongs to the Triassic landscape. It is one of a band with varying breadth from the south-eastern edge of the Black Forest on the Franconian Gäubucht up to Franconia in the north extending to Gäuflächen and passes north and east into the Bauland region, the Tauber Valley, and the Haller Plain. The Hohenlohe plane itself includes the area around the Kocher river and Jagst river, to the foot of the mountains and Keuper forest, and is a forest-poor and fertile old farmland.
In the subsurface are the layers of the Muschelkalk period, on the wide open spaces of layers of the Lower Keuper and are partially covered by loam. The most hard rock of the Muschelkalk in Tauber, Kocher, and its many tributaries of the Jagst river have cut and made it close, varied and scenic valley portions. The Gäufläche is framed in the southern semicircle of the forests of the Löwenstein, Waldburger Limpurger and mountains and dominates it.[7]
This Keuper perimeter dominates the Hohenlohe level by about 130 metres (430 ft), in Waldenburg even up to 180 metres (590 ft). The Stufenbildner is mainly on reeds, gravel and sandstone, because of waterlogging little, but are mainly forested. By fluvial erosion of the edge of the Keuper forest mountains over time has been divided into several sections with spur-like projections. In some places individual mountains were separated, at Öhringen: the Golberg (325 metres, 1,066 ft), the Verrenberg (205 m) and the Lindelberg (334 metres, 1,096 ft). The landscape around Öhringen shares two important elements of the Southwest German cuesta country: the Gäuplatten and the Keuper forest mountains.
The limestone in the subsurface of Hohenlohe and Haller is widely karstified, as evidenced by more than 2,000 sinkholes, many dry valleys and a few cave systems. In several limestone quarries, the rock is mined and usually broken into gravel, even in the town of Öhringen (at Unterohrn). However, the limestone deposited in a little water-permeable layer nor Lower Keuper, which prevents a rapid infiltration of precipitation in the limestone. Moreover, as the Lower Keuper often has loess, this has created mineral-rich, arable soil easy to work with sufficient moisture.
The area surrounding Öhringen is strongly influenced by agriculture. Besides the cultivation of cereals, sugar beet, cabbage, corn, and rapeseed, the orchards and vineyards give the landscape for mi around its typical character.
Öhringen