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.
| Candidate MSL Landing Site in Northeast Syrtis Major: ESP_017498_1980 ESP_018566_1980 (Interval in Earth days: 84) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.52 | 76.9 | -8.1 | 12.23 | 45.4 | 46.2 |
| Hanging Valley and Terraces in Mangala Valles: ESP_017691_1735 ESP_017902_1735 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.18 | 209. | 6.65 | -2.54 | 56.9 | 57.9 |
| Northern Plains Craters: ESP_017386_2315 ESP_018019_2315 (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 | 51.23 | 248. | 1.71 | -13.4 | 43.3 | 45.2 |
| Mini-Chaos in Crater Floor: ESP_017459_1990 ESP_053827_1990 (Interval in Earth days: 2834) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 18.80 | 61.3 | -4.8 | -27.4 | 44.6 | 46.9 |
| Young Esker-Like Ridges in Tempe Terra: ESP_017477_2190 ESP_018545_2190 (Interval in Earth days: 83) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.42 | 287. | -6.9 | 8.883 | 41.9 | 43.8 |
| Central Peaks of Two Impact Craters: ESP_017437_1550 ESP_017859_1550 (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 | -24.9 | 306. | 9.49 | -8.80 | 68.6 | 70.7 |
| Polygonal Ridges : ESP_017348_1910 ESP_018548_1910 (Interval in Earth days: 93) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 10.78 | 212. | 3.20 | -21.0 | 46.7 | 51.2 |
| Gully Landforms in Aram Chaos: ESP_017528_1830 ESP_018596_1830 (Interval in Earth days: 83) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.770 | 339. | -6.7 | 15.40 | 52.0 | 51.9 |
| Viscous Flow in Protonilus Mensae: ESP_017024_2230 ESP_017314_2230 (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 | 42.61 | 55.3 | -10. | 8.248 | 42.7 | 40.9 |
| Light-Toned Rocks inside a Crater: ESP_017292_1680 ESP_025375_1680 (Interval in Earth days: 630) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -11.8 | 304. | -4.3 | 26.62 | 59.6 | 50.6 |
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