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.
| Stepped Fan: ESP_011863_1715 ESP_012008_1715 (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 | -8.51 | 200. | 1.55 | 16.71 | 56.5 | 54.6 |
| 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 |
| Central Uplift and Pitted and Ponded Material in Well-Preserved Crater: ESP_011761_1485 ESP_011827_1485 (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 | -31.2 | 108. | -4.3 | -23.2 | 59.6 | 60.4 |
| 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 |
| Big Central Uplift of a Large Crater: PSP_010877_1610 ESP_028349_1610 (Interval in Earth days: 1361) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -18.8 | 120. | 5.24 | -14.3 | 62.0 | 61.8 |
| Branched Features on the Floor of Antoniadi Crater: ESP_012435_2015 ESP_012725_2015 (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 | 21.35 | 61.2 | -4.6 | 19.79 | 65.9 | 63.9 |
| Clays and Other Hydrated Materials in Sirenum Fossae Region: PSP_010888_1510 ESP_055392_1510 (Interval in Earth days: 3468) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -28.6 | 181. | 2.24 | -21.7 | 66.3 | 60.6 |
| Plains Near Valles Marineris: PSP_010580_1630 ESP_052605_1630 (Interval in Earth days: 3275) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -17.0 | 309. | 0 | -27.6 | 62.9 | 62.7 |
| Escarpment with Possible Clays: PSP_010460_2055 ESP_016684_2055 (Interval in Earth days: 485) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 25.33 | 339. | 7.92 | -9.96 | 50.6 | 41.5 |
| Light-Toned Layered Deposits on Southern Mid-Latitude Crater Floor: ESP_011310_1395 ESP_011811_1395 (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 | -40.1 | 182. | 2.14 | 23.84 | 67.1 | 59.0 |
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