Geodetic measurement of the local elastic response to the changing mass of water in Lago Laja, Chile
A geodetic station (ANTC) built in bedrock in southern Chile is undergoing non-steady vertical motion within a range of nearly 50 mm. These fluctuations are dominated by the earth's local elastic response to the changing weight of water in a reservoir located about 20 km away. There is also an annual periodic component of motion that is attributed to global and regional patterns of loading, as well as a steady tectonic signal. The local loading response constrains the average elastic structure of the area, and implies a stiffness that falls near the lower end of the range observed in rock samples. © 2003 Elsevier B.V. All rights reserved.
Physics of the Earth and Planetary Interiors
Bevis, M., Kendrick, E., Cser, A., & Smalley, R. (2004). Geodetic measurement of the local elastic response to the changing mass of water in Lago Laja, Chile. Physics of the Earth and Planetary Interiors, 141 (2), 71-78. https://doi.org/10.1016/j.pepi.2003.05.001