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.
| Clay Minerals in Nili Fossae: PSP_007358_2015 PSP_008215_2015 (Interval in Earth days: 67) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 21.25 | 78.4 | 7.89 | -7.09 | 39.1 | 43.4 |
| Exposure of High-Latitude Polar Layered Deposits Not Well Observed: PSP_005157_0875 PSP_005577_0925 (Interval in Earth days: 32) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.2 | 152. | 0 | 14.21 | 71.5 | 75.0 |
| Debris Apron Terminus: PSP_005353_1330 PSP_005630_1330 (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 | -46.8 | 111. | 0 | -22.4 | 42.0 | 46.6 |
| Fresh Pit Crater on Arsia Mons: PSP_004913_1735 PSP_005836_1735 (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 | -6.31 | 239. | -8.9 | 1.393 | 39.5 | 33.4 |
| 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 |
| Good-Looking Gullies: PSP_004777_1090 PSP_004843_1090 (Interval in Earth days: 5) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -70.6 | 2.11 | 5.76 | -2.69 | 53.2 | 54.0 |
| East Candor Region: PSP_004410_1735 ESP_012229_1735 (Interval in Earth days: 609) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.22 | 290. | 0.51 | -28.0 | 44.7 | 57.4 |
| Margin of South Polar Layered Deposits: PSP_005025_0975 PSP_005262_0975 (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 | -82.2 | 88.9 | -4.3 | 12.29 | 64.5 | 66.2 |
| Layered Sediments in Tithonium Chasma: PSP_005281_1750 PSP_005703_1750 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.92 | 270. | 10.9 | -5.09 | 35.2 | 34.1 |
| 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 |
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