Planned stereo pairs have suitable stereo convergence angles and illumination by design.
In addition to planned stereo pairs, the Pairendipity software can identify overlapping
HiRISE images that are serendipitously suitable for stereo processing and find stereo
pairs within the CTX dataset.
Planned HiRISE stereo pairs are listed in the “Stereo Pair List (CSV)” link below.
Since this list is based on produced stereo anaglyphs it also contains a few serendipitous
pairs that underwent special processing. Most serendipitous HiRISE stereo pairs are listed
in the “Pairendipity Stereo” link, while CTX stereo pairs are listed
in “Pairendipity CTX Stereo”.
Images taken close together in time minimize illumination and frost differences and are
especially useful (see the Delta-Days column in the Pairendipity files or difference
the orbit numbers in the image IDs in the Stereo Pair List file). Stereo pairs
with both images planned within the same 14-day (168-orbit) operations cycle are known as SPORCs.
| Central Peak of Well-Preserved Unnamed Crater: PSP_006782_1630 PSP_006927_1630 (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 | -16.7 | 331. | -6.1 | 5.697 | 45.0 | 46.2 |
| Layers in Memnonia Sulci: PSP_006616_1730 ESP_024285_1730 (Interval in Earth days: 1377) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.70 | 182. | -4.8 | 22.96 | 38.8 | 35.4 |
| Geologic Contact between Wallrock and Light-Toned Layered Deposits: PSP_005979_1710 PSP_006757_1710 (Interval in Earth days: 60) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.80 | 294. | 3.73 | -24.0 | 33.5 | 42.6 |
| Columnar Jointing Exposed in An Impact Crater in Marte Vallis: PSP_006774_2020 PSP_007341_2020 (Interval in Earth days: 44) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 21.57 | 184. | 7.5 | -9.82 | 38.5 | 40.5 |
| Exposure of Polar Layered Deposits in Area Poorly Observed: PSP_005715_0930 PSP_005951_0930 (Interval in Earth days: 19) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.1 | 19.3 | -0.0 | 13.96 | 78.8 | 81.0 |
| Polar Layered Deposit Stratigraphy Near Chasma Australe: PSP_004801_0950 PSP_005051_0950 (Interval in Earth days: 20) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.1 | 95.0 | 0.80 | 15.92 | 64.9 | 65.9 |
| Faults in Melas Chasma Wall: PSP_004977_1695 PSP_005478_1695 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -10.2 | 291. | -3.4 | 19.19 | 37.0 | 31.8 |
| Small Crater Filled By Deltaic Deposits: PSP_006954_1885 ESP_016250_1885 (Interval in Earth days: 724) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 8.520 | 312 | -0.3 | -27.7 | 38.5 | 44.0 |
| Gullies with Bright Color Deposits: PSP_005082_1365 ESP_012703_1365 (Interval in Earth days: 594) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -43.0 | 309. | -0.9 | 23.99 | 38.4 | 46.0 |
| Contact between Polygon and Massif: PSP_005700_2200 ESP_011818_2200 (Interval in Earth days: 477) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 39.77 | 346. | 0 | -24.3 | 59.2 | 72.7 |
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