Resumen en inglés

The San Diego mud volcano is located in Canalete, Córdoba, the object of this research, which aims to characterize the present geoforms. Leaks such as gryphons (splatters , bubblers , clast-rich,and extintic), sauces, and pools, deposits such as flows (old and recent) were found. The characterization of these geoforms was carried out by means of images taken through drones and field visits, thus obtaining a geomorphological cartography at a scale of 1: 500, managing to determine the largest number of geoforms in the study area to make a correlation between them and the occurrence of possible threats, It was established that splatters gryphons are associated with fire threats due to the amount of gases that they expel to the surface, bubblers gryphons and sauces were related to threats due to expulsion of mud and clastic taps to threats due to expulsion of a mud gap.