skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Geophysical characteristics of the hydrothermal systems of Kilauea volcano, Hawaii

Journal Article · · Geothermics (International Journal of Geothermal Research and its Applications); (United States)
 [1]
  1. Hawaiian Volcano Observatory, Hawaii National Park, HI (United States)

Clues to the structure of Kilauea volcano can be obtained from spatial studies of gravity, magnetic, and seismic velocity variations. The rift zones and summit are underlain by dense, magnetic, and seismic velocity variations. The rift zones and summit are underlain by dense, magnetic, high P-wave-velocity rocks at depths of about 2 km less. The gravity and seismic velocity studies indicate that the rift structures are broad, extending farther to the north than to the south of the surface features. The magnetic data allow separation into a narrow, highly-magnetized, shallow zone and broad, flanking, magnetic lows. The patterns of gravity, magnetic variations, and seismicity document the southward migration of the upper east rift zone. Regional, hydrologic features of Kilauea can be determined from resistivity and self-potential studies. High-level groundwater exists beneath Kilauea summit to elevations of +800 m within a triangular area bounded by the west edge of the upper southwest rift zone, the east edge of the upper east rift zone, and the Koa'e fault system. High-level groundwater is present within the east rift zone beyond the triangular summit area. Self-potential mapping shows that areas of local heat produce local fluid circulation in the unconfined aquifer (water table). Shallow seismicity and surface deformation indicate that magma is intruding and that fractures are forming beneath the rift zones and summit area. Heat flows of 370--820 mW/m[sup 2] are calculated from deep wells within the lower east rift zone. The estimated heat input rate for Kilauea of 9 gigawatts (GW) is at least 25 times higher than the conductive heat loss as estimated from the heat flow in wells extrapolated over the area of the summit caldera and rift zones. 115 refs., 13 figs., 1 tab.

OSTI ID:
5569857
Journal Information:
Geothermics (International Journal of Geothermal Research and its Applications); (United States), Vol. 22:4; ISSN 0375-6505
Country of Publication:
United States
Language:
English

Similar Records

Three-dimensional crust and mantle structure of Kilauea Volcano, Hawaii
Journal Article · Thu Nov 10 00:00:00 EST 1977 · J. Geophys. Res.; (United States) · OSTI ID:5569857

Geology of Kilauea volcano
Journal Article · Sun Aug 01 00:00:00 EDT 1993 · Geothermics (International Journal of Geothermal Research and its Applications); (United States) · OSTI ID:5569857

Modeling the three-dimensional structure of macroscopic magma transport systems: Application to Kilauea volcano, Hawaii
Journal Article · Mon Aug 10 00:00:00 EDT 1981 · J. Geophys. Res.; (United States) · OSTI ID:5569857