Based on theoretical considerations, basaltic volcanism of explosive character should be common on Mars. Although the record of explosive volcanic fields on Mars continues to grow, many unexplored volcanic fields remain. In this research, we identified a group of 25 volcanic cones and associated lava flows emplaced in the Noctis Fossae region on Mars. To analyze this volcanic field, we used images from the Context Camera (CTX) and High Resolution Imaging Science Experiment (HiRISE) of Mars Reconnaissance Orbiter (MRO). We interpreted those volcanic cones and their geological history by (1) analyzing their spatial distribution, (2) determining the morphometric parameters, (3) measuring orientations of their summit alignments, and (4) dating these cones along with surrounding lava flows. The identified cones are characterized by various states of preservation from almost fully eroded vent relicts to well-preserved edifices of conical shapes accompanied by short-distance lava flows. Morphological data suggest that the whole set of identified cones likely represent explosive scoria cones. Using the crater count dating method coupled with the structural relationship between the lava flows and volcanic cones, we found that the southern and central cones likely formed >300 Ma, while the northernmost cones between 200 and 50 Ma. These results suggest long-lived volcanism in the studied area active until the latest Amazonian period. In addition, to the present state of knowledge, these cones represent the youngest explosive volcanism in Tharsis and support other findings of young explosive-origin features on Mars. This might shed new light on the magmatic plumbing system of the Tharsis region, although magma sources from Syria Planum, or less likely Valles Marineris, are not excluded. Such magmas of explosive nature are probably rich in volatiles, which might derive from water and/or hydroxyl bearing minerals' or subsurface permafrost deposits. In addition, these magmas might be associated with intensive hydrothermal activity in the region.
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