LITHOLOGY OF THE COMPOSITION AND DISTRIBUTION OF GEOLOGICAL STRUCTURES ON CUMBRI HILL, BITING DISTRICT, PONOROGO REGENCY, EAST JAVA
DOI:
https://doi.org/10.33579/krvtk.v11i1.6414Keywords:
Cumbri Hill, trachyte, rudstone, structural geology, left slip faultAbstract
Cumbri Hill, situated on the boundary of Ponorogo and Wonogiri, is a narrow ridge trending northeast-southwest, formed by regional structures and variations in lithological resistance; however, comprehensive geological investigations remain scarce. This study seeks to determine the constituent lithology and examine the geological structural factors that affect the morphology of Cumbri Hill. The methodologies employed encompass geological mapping, petrographic and micropaleontological analyses, and stereonet analysis of fracture and fault data. The findings reveal that the lithology comprises rudstone limestone from the Middle Miocene (N16) within a Middle Neritic setting, which is subsequently overlain by shallow trachyte intrusions exhibiting porphyritic-vesicular textures. The geological structure is characterized by NE-SW oriented left-lateral strike-slip faults, with one site indicating a reverse left-slip mechanism attributed to a localized compressional component. This structural pattern governs the orientation of the ridge, linear valleys, and the location of the intrusion. The research findings significantly enhance the comprehension of the local magmatic and tectonic evolution of Ponorogo and act as a reference for advancing geological studies and geotourism in the area.
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