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. 2020 May 4;28(5):1871–1890. doi: 10.1007/s10040-020-02153-7

Fig. 7.

Fig. 7

a P-wave velocity models (RMS = 1.8 ms) and b resistivity model (absolute error = 4.8%) along the portion of Line 1 crossing talus deposits. Annotations indicate the locations of: springs (blue circle), tie points with other lines as numbered in Fig. 3 (grey, numbered boxes), and convergent flow paths (black ellipses). A sample of GPR data showing the differences in texture near the base of the Central Cone (c) and between the west and Central Cone (d)