| Coneto de Comonfort | |
| Settlement Type: | Municipal seat and city |
| Pushpin Map: | Mexico |
| Pushpin Label Position: | above |
| Pushpin Mapsize: | 300 |
| Pushpin Map Caption: | Location in Mexico |
| Subdivision Type: | Country |
| Subdivision Name: |  Mexico |
| Subdivision Type1: | State |
| Subdivision Name1: | Durango |
| Subdivision Type2: | Municipality |
| Subdivision Name2: | Coneto de Comonfort |
| Population As Of: | 2015 |
| Population Total: | 858 |
| Population Blank1 Title: | Ethnicities |
| Population Blank2 Title: | Religions |
| Coordinates: | 24.9833°N -160°W |
| Elevation M: | 1960 |
Coneto de Comonfort is a town and seat of the municipality of Coneto de Comonfort, in the state of Durango, north-western Mexico.[1] As of 2015, the town of Coneto de Comonfort had a population of 858.[2] The town has many desposits of quartz and stone.
Founded over 450 years ago, the town of Coneto de Comonfort was originally established as a mining community. It is located in the heart of the Coneto Mining District in the "Mexican Silver Trend", on the Mesa Central, east of the Sierra Madre Occidental mountains. This epithermal gold and silver-rich district has a long history of exploration and small scale production, dating back to the mid 16th century. The district has been explored by Orex Minerals Inc. (TSX.V: REX) and their project partner Fresnillo plc (LSE: FRES).
Gold and silver mineralization is hosted in over 40 epithermal quartz veins and breccias of low to intermediate sulfidation. A corridor of veining extends northwesterly for 17 km and has a width of about 4 km. Individual veins can be traced for up to 2 km and vary from 1 to 20 metres thick. These are exposed in an erosional window of Lower Volcanic Series (LVS) andesite domes, flows, tuff and agglomerate, surrounded by Upper Volcanic Series (UVS) rhyolites and dacites. The main silver-bearing mineral is acanthite and native gold is associated with hydrothermal hematite. The base metal minerals galena, sphalerite and minor chalcopyrite increase with depth. Associated with the mineralized structures are hydrothermal alteration zones, including kaolinitization, silicification, and pyritization.[3]