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.
| Eastern Side of Melas Region Basin with Light-Toned Layering: ESP_012005_1700 ESP_012638_1700 (Interval in Earth days: 50) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.81 | 283. | 1.82 | -19.8 | 55.7 | 52.4 |
| Iron and Magnesium Phyllosilicates in Terra Sabaea Crater Wall: ESP_012278_1695 ESP_066132_1695 (Interval in Earth days: 4196) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -10.2 | 31.3 | -3.6 | -22.5 | 54.2 | 48.1 |
| Streamlined Form and Channel Floor in Athabasca Valles: ESP_011825_1895 ESP_012814_1895 (Interval in Earth days: 77) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 9.439 | 156. | -3.5 | -16.8 | 59.8 | 59.0 |
| Unusual and Pristine Crater Morphology: ESP_011717_1910 ESP_012429_1910 (Interval in Earth days: 55) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 10.63 | 224. | -6.7 | 14.06 | 59.9 | 59.2 |
| Light-Toned Outcrops: ESP_011937_1970 ESP_012214_1970 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 16.73 | 337. | 3.54 | -22.5 | 61.9 | 64.8 |
| Layered Deposit in an Arabia Region Crater: ESP_012385_1825 ESP_030648_1825 (Interval in Earth days: 1423) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.668 | 350. | -23. | -0.71 | 58.9 | 50.7 |
| Grand Canyon of Gale Crater: ESP_012340_1750 ESP_012195_1750 (Interval in Earth days: 12) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.18 | 137. | 5.40 | -12.9 | 54.3 | 56.5 |
| Folded Layered Deposits: ESP_012305_1865 ESP_012371_1865 (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 | 6.390 | 11.8 | 1.20 | -19.8 | 58.6 | 60.1 |
| Oudemans Crater Central Uplift: ESP_011676_1700 ESP_028449_1700 (Interval in Earth days: 1307) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.84 | 267. | -22. | 7.568 | 59.1 | 56.2 |
| Well-Preserved 6-Kilometer Diameter Impact Crater with Gullies: ESP_012300_1440 ESP_020871_1440 (Interval in Earth days: 668) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.7 | 154. | -7.5 | 9.261 | 53.3 | 53.5 |
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