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.
Mawrth Vallis Phillosilicate Layers: PSP_005819_2050 PSP_006742_2050 (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 | 24.68 | 339. | 3.35 | -7.74 | 46.6 | 40.7 |
Incised Distributary Fan at the Distal End of Lethe Vallis: PSP_006195_1845 PSP_007118_1845 (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 | 4.550 | 155. | 0 | -14.6 | 35.3 | 41.5 |
Light-Toned Layered Rock Outcrop in Ladon Vallis: PSP_006637_1590 ESP_023383_1590 (Interval in Earth days: 1305) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -20.8 | 330. | 7.10 | 20.68 | 44.1 | 31.2 |
Bright Gully Deposits in A Fresh Impact Crater: PSP_006922_2120 PSP_007067_2120 (Interval in Earth days: 12) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 31.87 | 102. | 1.45 | 11.11 | 42.0 | 40.7 |
Intersecting Troughs in Lycus Sulci: PSP_006285_2000 ESP_032789_2000 (Interval in Earth days: 2065) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 19.66 | 216. | 0 | -24.1 | 39.9 | 40.8 |
Lava Falls in Northern Kasei Valles: PSP_005610_2025 ESP_040659_2025 (Interval in Earth days: 2731) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 22.00 | 286. | -5.7 | 8.888 | 47.7 | 50.0 |
Deeply-Incised Channels in Mantled Crater Walls: PSP_006544_1460 PSP_010750_1460 (Interval in Earth days: 328) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -33.6 | 351. | 0 | -16.0 | 50.6 | 71.0 |
Giza Region Unfrosted: PSP_004736_0950 PSP_005119_0950 (Interval in Earth days: 30) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -84.8 | 65.7 | 1.48 | -14.5 | 64.0 | 68.7 |
Apparent Fluvial Channel at the Summit of Hecates Tholus: PSP_004982_2120 PSP_005259_2120 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 31.70 | 150. | -3.6 | -27.4 | 63.0 | 60.7 |
Dune Source in Newton Crater: PSP_006866_1375 ESP_015964_1375 (Interval in Earth days: 709) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -42.1 | 201. | -6.2 | 21.12 | 62.2 | 65.1 |
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