Temporal gravity and height changes of the Yellowstone caldera, 1977 - 1994

24Citations
Citations of this article
14Readers
Mendeley users who have this article in their library.

This article is free to access.

Abstract

This paper describes the longest record of gravity measurements in the area of the Yellowstone caldera, Wyoming. The temporal gravity changes, at the ±12 μGal (10-8 ms-2) precision level, are compared with changes in heights from leveling and GPS. The gravity field decreased across the caldera from 1977 to 1983 during the uplift and attained a maximum decrease of up to -60 ± 12 μGal along the Caldera axis. The gravity field then reversed polarity to increasing values, of up to 60 ± 12 μGal between 1986 and 1993. The ratio between height and gravity changes varied during the entire time, but converged over the latter period following the free-air gravity gradient. General ground deformation deduced from leveling showed caldera-wide uplift of ∼15 mm/a during the period of gravity decrease, then from leveling and GPS, subsidence of ∼ 25 mm/a during the gravity increase. Copyright 1997 by the American Geophysical Union.

Cite

CITATION STYLE

APA

Arnet, F., Kahle, H. G., Klingelé, E., Smith, R. B., Meertens, C. M., & Dzurisin, D. (1997). Temporal gravity and height changes of the Yellowstone caldera, 1977 - 1994. Geophysical Research Letters, 24(22), 2741–2744. https://doi.org/10.1029/97GL02801

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free