Cârloman Hill

The Stânişoara Mountains constitute a well-individualized unit within the Piatra-Neamţ city, including only their southern extremity. The main peak has a general NW-SE orientation, consistent with the geological structure. Marls, clayey and disodilic shales predominate here, sometimes covered by loessoid deposits. The same geological structure can be found on the Cârloman hill, the western extension of Cozla. The maximum altitude reaches 806 m in Prihodiște Peak.