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.
| Dark Deposits around a Volcanic Fissure Adjacent to Tharsis Tholus: ESP_030440_1945 ESP_030862_1945 (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 | 14.06 | 268. | -8.4 | -24.4 | 59.2 | 57.1 |
| Layers in a Crater in Nilosyrtis: ESP_025001_2255 ESP_025911_2255 (Interval in Earth days: 71) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 44.91 | 69.8 | -1.9 | -24.2 | 44.4 | 43.3 |
| Portion of Gale Crater Mound: ESP_030102_1750 ESP_030880_1750 (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 | -5.03 | 137. | 9.9 | -8.53 | 50.6 | 44.8 |
| Gullied Niquero Crater: ESP_030021_1410 ESP_030443_1410 (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 | -38.7 | 193. | 4.97 | -16.9 | 49.4 | 45.0 |
| Valleys with Layered Sediments along Uplands at Ladon Valles Basin: ESP_029871_1615 ESP_031084_1615 (Interval in Earth days: 94) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -18.5 | 326. | 5.61 | 27.24 | 50.1 | 34.7 |
| Candidate Future Landing Site in Sabrina Vallis Delta: ESP_029845_1920 ESP_029990_1920 (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 | 11.97 | 313. | -7.3 | 11.05 | 59.1 | 57.8 |
| Sediments within Valleys in Uplands Near Ladon Valles: ESP_030082_1615 ESP_030161_1615 (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 | -18.4 | 326. | -9.9 | 24.27 | 49.2 | 45.6 |
| Deposits Containing Gypsum along Melas Chasma Floor: ESP_030044_1710 ESP_030255_1710 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.85 | 282. | -0.7 | -15.6 | 50.7 | 50.2 |
| Gullies in Dunes on Kaiser Crater Floor: ESP_030067_1325 ESP_030133_1325 (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 | -46.9 | 19.4 | 2.97 | -16.0 | 50.9 | 51.3 |
| More Coverage of Distorted Layer in Noctus Labyrinthus: ESP_030071_1720 ESP_030216_1720 (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 | -8.10 | 265. | -9.3 | 1.688 | 51.3 | 49.4 |
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