The Bärental originates from the Franconian Alb, located approximately two kilometers northeast of Seubersdorf,[2] at an elevation of around 465 meters above sea level.

[2] This bend in the valley is marked by two distinctive natural formations, the Juraturm and Geierstein,[3] both of which are prominent rock needles, each standing at a height of 25 meters.

[2] Upon reaching Krassacher Mühle, the valley widens considerably,[2] which, according to the narrower definition, marks the conclusion of the Bärental, spanning approximately 3 kilometers.

[7] This is followed by the lower marl limestones of the same Malm strata,[3][7] although these are primarily concealed by debris and sedimentary deposits along the valley floor.

The initial section, commencing at the Krassacher Mühle, exhibits open meadows along the valley floor and a combination of mixed and deciduous forests at its edges.

[10] The slender thickets of alder, ash, and willow adorning the riverbanks serve as vestiges of the ancient floodplain forests.

[11] Ade conducted botanical research in the Weismain area during the early 20th century and provided the first comprehensive description of the indigenous flora.

Nestled upon the rocky needle Juraturm is an annually inhabited eyrie, which is easily visible from the hiking trail through the valley.

In order to ensure the safety of climbers in Bärental and Kleinziegenfelder Tal, a station and lodging are provided by the Kulmbach mountain rescue division, housed within an outbuilding of the mill.

[6] Bärental is visited by numerous hikers in spring, summer, and fall because of its quiet location and largely untouched nature.

[4] Additionally, the local mountain guard division stationed at Herbstmühle organizes the annual Juraturm festival on October 3.