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.
| Inverted Channel Floor in CTX Image: ESP_019249_1745 ESP_019394_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 | -5.80 | 154. | -11. | 4.813 | 57.4 | 56.0 |
| Cones in Isidis Planitia: ESP_019291_1965 ESP_019924_1965 (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 | 16.59 | 82.7 | 17.0 | 3.208 | 48.8 | 54.0 |
| Alluvial Fans in Crater: ESP_019489_1510 ESP_025291_1510 (Interval in Earth days: 452) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -28.5 | 84.0 | 4.07 | -20.3 | 66.3 | 63.8 |
| Central Peak in Crater on Rim of Sinai Planum: ESP_019456_1645 ESP_019601_1645 (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 | -15.3 | 263. | -4.0 | 13.69 | 60.4 | 58.6 |
| Bedrock in Hydrae Chasma: ESP_019336_1730 ESP_019969_1730 (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 | -6.75 | 297. | 8.78 | -6.40 | 56.2 | 56.2 |
| Lava Vent with Channels: ESP_019325_1960 ESP_019391_1960 (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 | 15.69 | 235. | 7.19 | -14.6 | 49.9 | 52.1 |
| Rim and Ejecta of Very Fresh 7-Kilometer Diameter Crater in Arcadia Region: ESP_019547_2335 ESP_024848_2335 (Interval in Earth days: 413) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 53.29 | 288. | 5.88 | -21.5 | 58.3 | 51.5 |
| Diverse Lithologies in Central Uplift of Stokes Crater: ESP_019380_2360 ESP_019604_2360 (Interval in Earth days: 18) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 55.59 | 171. | -16. | 10.82 | 58.7 | 59.7 |
| Well-Preserved 6-Kilometer Diameter Impact Crater: ESP_019371_1700 ESP_020571_1700 (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 | -9.81 | 63.1 | 4.37 | -11.4 | 57.7 | 55.3 |
| Bedrock in Walls of Well-Preserved Impact Crater in Tartarus Montes: ESP_019222_2055 ESP_019367_2055 (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 | 25.03 | 167. | -7.6 | 5.969 | 49.8 | 49.8 |
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