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.
| 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 |
| Fresh Small Rayed Crater: ESP_029908_1660 ESP_029974_1660 (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 | -13.7 | 34.2 | 22.6 | 1.785 | 48.9 | 50.0 |
| 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 |
| Central Peak and Layered Bedrock: ESP_030095_1615 ESP_030385_1615 (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 | -18.5 | 330. | 4.96 | 26.48 | 47.9 | 42.9 |
| Layer Exposures in Depression at Valley Terminus: ESP_029898_1765 ESP_039999_1765 (Interval in Earth days: 787) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -3.36 | 307. | 1.11 | 13.06 | 52.9 | 42.4 |
| 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 Southern Mid-Latitude Crater: ESP_029963_1385 ESP_030596_1385 (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 | -41.2 | 337. | 8.17 | -18.4 | 50.6 | 43.6 |
| 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 |
| Streamlined Form in Athabasca Valles: ESP_030009_1895 ESP_040176_1895 (Interval in Earth days: 793) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 9.475 | 156. | -1.3 | -16.8 | 57.5 | 49.5 |
| Cross Section of Hummocks in Atlantis Chaos: ESP_030061_1450 ESP_030351_1450 (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 | -34.8 | 181. | 3.29 | 22.25 | 48.3 | 42.7 |
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