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.
| Landslide Deposits Overlapping the Middle Mount of Coprates Chasma: PSP_008616_1685 PSP_009051_1685 (Interval in Earth days: 34) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -11.5 | 291. | -2.7 | 14.75 | 60.6 | 60.9 |
| Unnamed Well-Preserved Crater in Tyrrhena Terra: PSP_008544_1615 PSP_009335_1615 (Interval in Earth days: 61) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -18.4 | 98.9 | -6.3 | 11.96 | 65.1 | 66.0 |
| Light-Toned Rock and Scarps in MOC Images R10-03225 and R16-01292: PSP_008877_2165 PSP_009523_2165 (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 | 36.29 | 358. | -8.1 | 13.60 | 43.1 | 43.4 |
| Polar Layered Deposits Unconformity: PSP_009203_2625 PSP_009585_2625 (Interval in Earth days: 30) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 82.34 | 79.7 | -7.1 | 7.321 | 58.9 | 59.8 |
| Ejecta Flow around Obstacle in West Utopia Planitia: PSP_008755_2160 PSP_008966_2160 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 35.78 | 88.1 | 11.2 | -7.03 | 41.1 | 43.2 |
| Layered Deposits and Unconformities in Western Gemini Scopuli: PSP_009162_2630 PSP_009624_2630 (Interval in Earth days: 36) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.03 | 106. | 6.89 | -9.31 | 58.6 | 61.4 |
| Cones among the Tartarus Montes: PSP_008818_2055 PSP_009029_2055 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 25.15 | 169. | 6.65 | -10.6 | 43.2 | 45.3 |
| High-Latitude Exposure of North Polar Layered Deposits: PSP_009187_2680 ESP_018221_2680 (Interval in Earth days: 704) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.92 | 95.3 | -6.5 | -14.0 | 63.1 | 63.7 |
| Terraces in Reull Vallis Walls: PSP_008570_1410 PSP_010139_1410 (Interval in Earth days: 122) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.4 | 111. | -3.2 | 10.19 | 79.2 | 76.7 |
| Stratigraphy of Phyllosilicate Rocks Northwest of Nili Fossae: PSP_008993_2020 PSP_009626_2020 (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 | 21.82 | 72.2 | -1.3 | -22.6 | 45.2 | 49.0 |
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