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.
| Vent near Olympica Fossae: ESP_080130_2070 ESP_080407_2070 (Interval in Earth days: 21) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 26.88 | 247. | 4.53 | -6.84 | 47.0 | 49.3 |
| Polar Terrain Sample: ESP_080021_2575 ESP_079968_2575 (Interval in Earth days: 4) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 77.09 | 332. | -8.2 | 7.25 | 57.6 | 56.2 |
| Exposure of North Polar Layered Deposits: ESP_080023_2670 ESP_079391_2670 (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 | 86.96 | 247. | -8.9 | -21.8 | 63.2 | 62.6 |
| Layered Late-Stage Fan in Gale Crater: ESP_080187_1755 ESP_080332_1755 (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 | -4.26 | 137. | -23. | 0.545 | 61.2 | 59.5 |
| Crater Exposing Deposits in Candidate ExoMars Landing Site in Oxia Planum: ESP_080140_1980 ESP_079652_1980 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.61 | 335. | 1.31 | 15.69 | 49.7 | 47.2 |
| Crater Layers: ESP_080109_2570 ESP_080373_2570 (Interval in Earth days: 21) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 76.95 | 89.2 | -6.0 | -20.0 | 57.8 | 60.9 |
| Mound in Chryse Planitia: ESP_080180_2060 ESP_080246_2060 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 25.58 | 322. | 8.26 | -8.22 | 47.2 | 48.9 |
| Small Delta or Fan: ESP_080135_1830 ESP_080280_1830 (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 | 3.140 | 114. | -7.4 | 16.94 | 56.2 | 54.6 |
| Steep Polar Scarp and Dune Source in Western Olympia Cavi: ESP_080081_2635 ESP_080186_2635 (Interval in Earth days: 8) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.61 | 119. | -2.0 | 11.78 | 61.1 | 61.1 |
| Valleys along Lower Wallrock Slopes in Juventae Chasma: ESP_079825_1760 ESP_080313_1760 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.19 | 297. | -2.1 | -14.2 | 59.4 | 60.5 |
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