Tracking magma pathways and surface faulting in the Southwest Rift Zone and the Koa'e fault system (Kilauea volcano, Hawai 'i) using photogrammetry and structural observations.

ABSTRACT: Volcanic islands are often subject to flank instability, resulting from a combination of magmatic intrusions along rift zones and gravitational spreading causing extensional faulting at the surface. Here, we study the Koa'e fault system (KFS), located south of the summit caldera of Kīlauea volcano in Hawai'i, one of the most active volcanoes on Earth, prone to active faulting, episodic dike intrusions, and flank instability. Two rift zones and the KFS are major structures controlling volcanic flank instability and magma propagation. Although several magmatic intrusions occurred over the KFS, the link between these faults, two nearby rift zones and the flank instability, is still poorly studied. To better characterize the KFS and its structural linkage with the surrounding fault and rift zo

SUBMITTER: Mannini S 

PROVIDER: S-EPMC11008072 | biostudies-literature | 2024

REPOSITORIES: biostudies-literature