Insights on the state of stress in the mantle beneath Pahala, Hawai‘i

Magma supply rates from the mantle to Hawaiian volcanoes serve as an important control on eruptive behavior at the surface. The Pa ̄hala Sill Complex, a collection of magma-bearing, seismogenic structures at 40 km depth beneath Hawai‘i, presents an opportunity to elucidate interactions between stres...

Full description

Bibliographic Details
Published in:Volcanica
Main Authors: John D. Wilding, Zachary E. Ross
Format: Article
Language:English
Published: Volcanica 2024-01-01
Subjects:
Online Access:https://www.jvolcanica.org/ojs/index.php/volcanica/article/view/239