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.
| Rampart Crater Ejecta Exposed in Cross-Section: ESP_018017_1680 ESP_026799_1680 (Interval in Earth days: 684) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.1 | 310. | -0.4 | 10.24 | 61.6 | 60.0 |
| Fault in Ius Chasma: ESP_017939_1720 ESP_025231_1720 (Interval in Earth days: 568) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.89 | 279. | -3.1 | -22.3 | 59.0 | 50.2 |
| Disrupted Blocky Outcrop in Cerberus Palus: ESP_018036_1880 ESP_043710_1880 (Interval in Earth days: 2001) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 8.089 | 149. | -6.4 | 6.703 | 50.5 | 45.5 |
| Raised Polygonal Ridges and Light-Toned Material in Syrtis Region: ESP_018065_1975 ESP_019133_1975 (Interval in Earth days: 83) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.49 | 76.4 | -5.2 | 15.52 | 46.5 | 48.0 |
| Light-Toned Outcrops in Noctis Region: ESP_017979_1715 ESP_018401_1715 (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 | -8.26 | 267. | -7.1 | -21.7 | 59.6 | 60.6 |
| Small Channel in Elysium Planitia: ESP_017838_1865 ESP_017983_1865 (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 | 6.589 | 155. | -4.2 | 10.54 | 50.7 | 49.9 |
| Repeated Sulfate and Clay Beds in West Gale Crater: ESP_017786_1745 ESP_017931_1745 (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 | -5.36 | 137. | -13. | 1.249 | 57.9 | 57.2 |
| Crater Floor Depressions: ESP_017934_2025 ESP_018435_2025 (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 | 22.32 | 53.1 | -13. | 7.638 | 45.4 | 44.9 |
| Clay Diversity on Flank of Mawrth Vallis: ESP_017897_2045 ESP_018530_2045 (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 | 24.08 | 341. | 4.44 | -14.5 | 43.4 | 46.8 |
| Impact Crater Teetering on the Edge of a Canyon: ESP_017740_1680 ESP_025810_1680 (Interval in Earth days: 629) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -11.7 | 312. | 5.84 | -8.97 | 60.6 | 56.8 |
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