Kilauea Volcano, Hawai`i : Deformation

Kilauea Volcano, Hawai`i : Deformation

Electronic Tilt | Global Positioning System (GPS)

Note: Check the Photo Glossary or a good dictionary for any terms unfamiliar to you.

Map of selected deformation stations

Map showing location of deformation stations

Electronic Tilt

Graph of tilt at Uwekahuna and Pu`u `Ō `ō tiltmeter stations, Kilauea Volcano, Hawai`i

This graph shows the radial tilt at Uwekahuna (UWE), on the northwest rim of Kīlauea's caldera as recorded by continuously operating electronic tiltmeters. Positive changes often indicate inflation of the magma storage areas beneath the caldera, but may also result from heavy rainfall or, occasionally, instrumental malfunctions. The Y-axis is in microradians, an angular measure in parts per million; for example, one microradian represents the tilt of a 1-km-long bar, one end of which is lifted up or down 1 mm.

Data are shown for a one-week period. The electronic tilt display shows relative values rather than absolute values. In other words, we do not assign a specific value to any given time; rather, we look at the difference in tilt over a period of time (hours, days, weeks).

Global Positioning System (GPS)

Graph showing displacement between UWEV and AHUP GPS stations, Kīlauea Volcano, Hawai`i

This graph shows the change in distance between two Global Positioning System (GPS) stations located on opposite sides of Kīlauea's caldera. A rapid increase in distance can be interpreted as inflation of the summit magma reservoir. The graph is refreshed once per day.

For more information on how electronic tiltmeters and GPS receivers help monitor the deformation of Kīlauea and Mauna Loa volcanoes, see a summary of the inflation-deflation of magma chambers.

Eruption-viewing opportunities change constantly, so refer to this page often. Those readers planning a visit to Kīlauea or Mauna Loa volcanoes can get much useful information from Hawai`i Volcanoes National Park.