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.
| Surface of Debris Apron in Eastern Hellas Region : ESP_048960_1385 ESP_049105_1385 (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 | -41.3 | 104. | 1.84 | 14.82 | 35.1 | 34.3 |
| Gullies and Arcuate Ridges in Nereidum Montes : ESP_048623_1385 ESP_049124_1385 (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 | -41.2 | 307. | -23. | -8.80 | 38.3 | 35.9 |
| Fresh Rocky Crater in Acidalia Planitia : ESP_048872_2120 ESP_083977_2120 (Interval in Earth days: 2735) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 31.69 | 338. | -6.8 | 1.873 | 64.0 | 68.2 |
| The Changing Dunes of Wirtz Crater: ESP_021603_1315 ESP_021893_1315 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -48.2 | 334. | -20. | -0.50 | 47.9 | 42.8 |
| Bedrock Exhumed from the Deep: ESP_011523_1695 ESP_012367_1695 (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 | -10.5 | 123. | 0.75 | -21.5 | 57.7 | 54.8 |
| Eroded Scallops with Layers: PSP_001938_2265 PSP_002439_2265 (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 | 46.01 | 92.1 | -2.5 | 13.48 | 56.8 | 63.0 |
| Lava in Western Elysium Planitia : ESP_048286_1855 ESP_048497_1855 (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 | 5.395 | 139. | 20.3 | 2.836 | 48.9 | 48.2 |
| Cones and Channels East of Olympus Mons : ESP_048243_1980 ESP_048454_1980 (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 | 17.76 | 232. | 11.3 | -6.93 | 57.7 | 57.4 |
| Hanging Valleys in Dao Vallis : ESP_048222_1445 ESP_048789_1445 (Interval in Earth days: 45) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.3 | 91.0 | 28.1 | 10.98 | 37.1 | 33.1 |
| Crater Wall with Flow Lineae in Terrain North of Morava Valles : ESP_048424_1690 ESP_062969_1690 (Interval in Earth days: 1134) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -10.9 | 334. | -0.7 | 8.839 | 40.7 | 59.4 |
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