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.
| Northern Plains Craters: ESP_026446_2305 ESP_027158_2305 (Interval in Earth days: 55) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 50.09 | 219. | 0 | 16.82 | 42.3 | 43.0 |
| Complex Superposition of Fractures: ESP_026286_2235 ESP_026563_2235 (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 | 43.31 | 269. | -3.0 | -21.3 | 41.0 | 43.0 |
| Fresh Crater: ESP_026365_2260 ESP_027710_2260 (Interval in Earth days: 105) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 45.42 | 271. | 1.37 | 20.86 | 41.0 | 45.7 |
| Exposure of Nili Fossae Megabreccias: ESP_026346_2000 ESP_026491_2000 (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 | 19.73 | 74.0 | 1.32 | 16.62 | 42.9 | 42.0 |
| Bedform Changes Southwest of Schiaparelli Crater: ESP_026322_1720 ESP_027166_1720 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.72 | 13.0 | -3.6 | -18.2 | 56.9 | 59.2 |
| Southern Ladon Basin near the Mouth of Ladon Valles: ESP_026139_1600 ESP_027616_1600 (Interval in Earth days: 115) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -19.8 | 329. | 5.17 | -12.8 | 63.6 | 65.3 |
| How Did Valles Marineris Form?: ESP_025415_1675 ESP_026259_1675 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.3 | 294. | 0 | -17.9 | 53.1 | 60.5 |
| A Volcanic Pit Chain and Dust Avalanches : ESP_026249_2025 ESP_026750_2025 (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 | 22.26 | 202. | -7.3 | 17.82 | 42.6 | 41.8 |
| Fan with Light-Toned Deposits: ESP_025990_1995 ESP_026135_1995 (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 | 19.10 | 76.1 | -27. | -15.8 | 44.5 | 43.8 |
| Light-Toned Hydrated Material along Melas Chasma Wallrock and Floor: ESP_026088_1710 ESP_026022_1710 (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 | -9.11 | 282. | -11. | 12.10 | 57.1 | 55.2 |
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