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.
| 12-Kilometer Diameter Crater with Multiple Pronounced Internal Morphologies: ESP_033317_1945 ESP_033462_1945 (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 | 14.33 | 199. | -1.3 | 12.06 | 37.2 | 36.6 |
| Floor of Mclaughlin Crater: ESP_033391_2020 ESP_037149_2020 (Interval in Earth days: 293) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 21.90 | 337. | 1.00 | 18.02 | 38.3 | 51.1 |
| Layered Materials on Northeast Hellas Planitia Rim: ESP_033348_1525 ESP_033282_1525 (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 | -27.2 | 78.2 | -4.0 | 18.08 | 52.0 | 49.5 |
| Exposures of Light-Toned Layered Material along Ladon Valles Floor: ESP_033431_1585 ESP_033365_1585 (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 | -21.2 | 331. | 0.00 | 22.10 | 49.2 | 46.7 |
| Light-Toned Layered Deposits in Uplands West of Ladon Valles Basin: ESP_033352_1605 ESP_033774_1605 (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 | -19.4 | 327. | 4.51 | -10.4 | 46.7 | 53.6 |
| Differential Compaction around a Crater Peak: ESP_033108_1800 ESP_033253_1800 (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 | -0.12 | 146. | 6.22 | 18.28 | 36.0 | 36.3 |
| Possible Terraced Crater in Arcadia Planitia: ESP_033079_2280 ESP_033356_2280 (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 | 47.51 | 211. | 4.74 | -16.7 | 52.2 | 50.9 |
| Impact Crater with Central Peak: ESP_033202_1685 ESP_060393_1685 (Interval in Earth days: 2119) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -11.5 | 101. | 2.77 | -6.13 | 40.8 | 49.3 |
| Possible Lake Margin in Shalbatana Vallis: ESP_032904_1835 ESP_033537_1835 (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 | 3.523 | 316. | 5.31 | -26.9 | 34.5 | 41.8 |
| Central Peak of Taxco Crater: ESP_033273_2010 ESP_042095_2010 (Interval in Earth days: 687) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 20.64 | 319. | -3.3 | 11.76 | 38.3 | 37.9 |
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