In addition to planned stereo pairs, the Pairendipity software can identify all overlapping images suitable for stereo processing. Global lists of such image pairs for the HiRISE and CTX datasets are provided here ordered by latitude. Images taken close together in time minimize illumination and frost differences and are especially useful (see the Delta-Days column). Stereo images planned within the same 14-day operations cycle are known as SPORCs.
Kunowsky Crater Central Peak with Strong Olivine Signature: ESP_016235_2370 ESP_016314_2370 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 56.79 | 350. | 8.37 | 25.32 | 50.4 | 48.5 |
Layers in Trough Floor and Scarp of Western Bench of Terby Crater: ESP_016206_1525 ESP_016351_1525 (Interval in Earth days: 11) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -27.4 | 74.5 | 8.70 | 23.26 | 59.0 | 59.9 |
Layering in Hellas Planitia: ESP_016299_1420 ESP_019978_1420 (Interval in Earth days: 287) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.4 | 57.0 | 7.21 | -12.1 | 67.3 | 67.2 |
Potential MSL Landing Site in Eberswalde Crater: ESP_016065_1560 ESP_016210_1560 (Interval in Earth days: 11) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -23.9 | 326. | -28. | -15.6 | 57.2 | 58.1 |
Possible Small-Scale Tributary into Reull Vallis: ESP_016297_1415 ESP_019765_1415 (Interval in Earth days: 270) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.2 | 111. | 8.34 | -8.43 | 67.8 | 69.6 |
Juventae Chasma: ESP_016145_1775 ESP_017424_1775 (Interval in Earth days: 100) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -2.49 | 298. | -12. | 7.841 | 45.5 | 53.7 |
Lineated Valley Fill Near Deuteronilus Region: ESP_016168_2180 ESP_024594_2180 (Interval in Earth days: 656) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 37.78 | 23.8 | 4.56 | -7.15 | 42.2 | 43.8 |
Massif with Radial Troughs in Viking 072A02: ESP_016011_2185 ESP_016499_2185 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.06 | 347. | 25.6 | 2.429 | 41.2 | 41.5 |
Stranded Lobe of Material with Associated Ridge on Valley Floor: ESP_016238_2180 ESP_017161_2180 (Interval in Earth days: 72) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 37.54 | 273. | -3.4 | 6.789 | 42.5 | 40.5 |
Sinuous Ridges in the Aeolis and Zephyria Regions: ESP_016282_1750 ESP_016915_1750 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.04 | 155. | 22.5 | 8.613 | 45.4 | 52.2 |
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