Table 2

Characteristics of the largest mass loss features observed in Anhur.

Landmark OSIRIS F22 image Δ (km) m px−1 h (m) i (deg) Lsha (m)
Dust bank (Region 1, Fig. 3) NAC_2016-02-10T08.14.06.243Z 50.06 0.937 14 ± 2 42 ± 6 12.9 ± 1.5
New scarp (Region 1, Fig. 2) NAC_2016-02-10T08.14.06.243Z 10 ± 2 52 ± 12
Z2 (Region 2, Fig. 7) NAC_2015-03-25T13.58.49.354Z 87.37 1.64 8.6 − 26.8 63 ± 18
New cliff (Region 4, Fig. 10, A3) NAC_2016-02-10T08.14.06.243Z 49.91 0.934 9 ± 2 45 ± 11 9 ± 2
Cliff retreat (Region 4, Fig. 10) NAC_2015-03-25T13.23.48.562Z 87.67 1.64 4 ± 2 76 ± 1 14 ± 3

Landmark Length (m) Width (m) Area (m2) Volume (m3) Mass (kg)

Dust bank (Region 1, Fig. 3) 116 ± 2 (53 − 73) ± 2 949 13145 7.0 × 106
New scarp (Region 1, Fig. 2) 26 ± 2 12 ± 2 327.5 3144 1.7 × 106
Z2 (Region 2, Fig. 7, A3) 92 ± 4 (17 − 25) ± 4 1.9 × 107
New scarp in Bes* (Region 3, Figs. 8, and 9) 140 ~5000 50000 2.6 × 107
New cliff (Region 4, Fig. 10, A3) (36∕44) ± 2 (9.1∕24.3) ± 2 215/437 1920/3840 1−2 × 106
Cliff retreat (Region 4, Fig. 10, A2) 9 ± 4 15 ± 4 43 153 8.2 × 104

Notes. Z2is the structure observed in 2015 and reported in Fig. 7. (*) we also report the estimation from Fornasier et al. (2017) for the new scarp in Bes region, nearby the Anhur-Bes boundary.

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