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.
| Look for Change Caused By Mass Wasting Since 2007: PSP_009648_2650 PSP_010097_2650 (Interval in Earth days: 35) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.99 | 151. | 2.16 | -12.3 | 62.3 | 67.1 |
| Exposure of Polar Layered Deposits: PSP_010116_2680 PSP_010075_2720 (Interval in Earth days: 3) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 88.20 | 303. | -10. | -10.3 | 69.5 | 69.6 |
| Layering in North Polar Layered Deposit Trough: PSP_010261_2595 PSP_010525_2595 (Interval in Earth days: 20) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 79.12 | -0.9 | -4.3 | -18.3 | 65.1 | 69.8 |
| Impact Crater on Lava Flow Front in Amazonis Planitia: PSP_010109_1975 ESP_053848_1975 (Interval in Earth days: 3408) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.14 | 204. | -6.4 | 7.576 | 50.7 | 44.4 |
| Clays Exposed in Channels along West Ladon Valles: PSP_010342_1600 ESP_034552_1600 (Interval in Earth days: 1886) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -19.6 | 327. | 0.85 | -19.2 | 65.0 | 63.0 |
| Exposure of North Polar Basal Unit: PSP_009945_2645 PSP_010063_2645 (Interval in Earth days: 9) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.40 | 343. | -12. | 3.559 | 65.2 | 65.5 |
| Western Rim and Ejecta of Very Young 12-Kilometer Diameter Crater: PSP_009810_2140 PSP_010443_2140 (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 | 33.45 | 84.2 | 7.72 | -5.93 | 45.6 | 51.8 |
| Layering Under Crater Ejecta: PSP_009324_1830 ESP_020374_1830 (Interval in Earth days: 861) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 3.065 | 37.4 | 2.15 | 20 | 53.7 | 53.6 |
| Unconformity in Gemina Lingula Layered Deposits: PSP_010088_2610 PSP_010827_2610 (Interval in Earth days: 58) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 80.70 | 32.6 | 6.60 | -18.7 | 63.2 | 75.4 |
| Well-Preserved Crater on a Steep Slope in Tyrrhena Terra: PSP_009824_1610 PSP_010246_1610 (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 | -18.5 | 69.0 | 6.12 | -5.57 | 65.8 | 65.3 |
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