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We first show that the GPS-derived strain rates at Long Valley are consistent with regional tectonic patterns in strain rate. The GPS-derived strain rates decline in the northeast-southwest direction and increase in the northwest-southeast direction. The northeast-southwest decline matches the west-toward-east movement of the Sierra Nevada. Similarly, the northwest-southeast increase matches the east-toward-west movement of the Sierra Nevada. We also observe a rapid increase in strain rate in a northwest-southeast direction at the northern end of the caldera, which is consistent with the presence of the north-south trending Walker Lane fault. The strain rates near Long Valley also show the presence of a ~9.2 km long northwest-southeast trending shear zone that is consistent with regional tectonic transtension. These GPS-derived strain rates are compared to the strain rates from the regional plate-bounding SRTM velocity model, which is also used in the GPS-derived strain rates. The comparison of the GPS-derived and SRTM-derived strain rates shows good agreement across the caldera. The GPS-derived strain rates from the SRTM velocity model also show good agreement with the GPS-derived strain rates in the northwest-southeast direction. Therefore, we conclude that the GPS-derived strain rates are consistent with the SRTM-derived strain rates. Lastly, we identify repeating patterns in the GPS-derived strain rates that are consistent with the regional tectonic strain rates. The strain rates in the northwest-southeast direction are roughly double the strain rates in the northeast-southwest direction. This is consistent with a structural model that assumes that a compressive strain field that decreases from northeast to southwest is balanced by a tensile strain field that increases from northeast to southwest. The large northwest-southeast gradient in strain rate that we observe is also consistent with the compressive strain field, which is inferred from a structural model of the crust, which also shows a similar northwest-southeast gradient.

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