Extended Data Table 1 A matrix of Eros geologic observations that can be explained with a given mechanism or combination of mechanisms

From: Seismic resurfacing of 433 Eros indicative of a highly dissipative interior for large near-Earth asteroids

  1. The transition between small and large craters is at approximately 500 m. The observations and modeling suggest that this demarcation is not so starkly defined and there exists a transition region between 250 and 500 m. However, for the purposes of this exercise, it is useful to define a clear transition where the differences in geologic properties are clearly observed.
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