Tectono-geomorphic landforms, which are the tools used in the definition and interpretationof faulting, can serve as the enlightenment of regional tectonic processes as well asproviding topographic landscape richness. These shapes are among the main referencesources for the reflection of tectonic movements on topography in active fault zones. In thisstudy, it was prepared for tectono-geomorphic shapes in Balıkgöl and its environment, whichare controlled by the Balıkgöl Fault Zone. Balıkgöl is located between Ağrı and Iğdırprovinces in Eastern Anatolia. Here, there are Perilidağ, Canderviş, Yeniçadır Dağı andKovancık fault segments belonging to the Balıklıgöl Fault Zone. Many tectono-geomorphicforms have developed in the topography with the effect of these fault segments. Offsetvalley, fault lake, pressure ridge, linear ridge, shutter ridge, triangular surface (facet), hangingvalley, beheaded valley, fault wedge basin, fault steepness, fault steps, alluvial fan,sequential water springs, hooked drainage samples, parallel drainage and landslides are themain structures seen in the research area and shed light on faulting. Based on thesestructures, the segments formed by the fault zone were examined and to contribute to thetectonic geomorphology literature of the Balıklıgöl Fault Zone.