أثر العمليات الجيومورفية في تشكيل كهف (كونبا)‎ جبل كولان في محافظة السليمانية

Abstract EN

Field hydrogeographic evidence indicates that the Konba cave originated during the third and fourth time and as a result of geological، hydrological and climatic factors, and what morphodynamic and morphodynamic processes only tools worked on the decomposition، disintegration and melting of rocks that produced geomorphological shapes، as it is necessary to study and analyze the types of rocks and their meltability because of its impact on the emergence and development of the cave، and the cave of Kunba is a natural cavity interspersed with cavities and internal caves of varying sizes, the cave has been classified into two wings (right and left) from which three main cavities branch Compatible with the three aquatic feeding phases (frequent water feeding، dampening، and aqueous leaching)، these chambers can be classified as geomorphic safeness except for specific and scattered locations within the cave of the area.