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.
| Unconformity in Gemini Lingula Layered Deposits: PSP_009482_2605 PSP_009878_2605 (Interval in Earth days: 31) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 80.31 | 22.5 | -0.8 | -19.1 | 58.4 | 62.7 |
| Ejecta Flow Around Obstacles in Eastern Elysium Region: PSP_010018_2000 PSP_010519_2000 (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 | 19.94 | 168. | -4.6 | 18.56 | 49.5 | 50.4 |
| Mounds in Ulysses Fossae: PSP_009409_1860 PSP_009554_1860 (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 | 5.804 | 237. | -7.2 | 8.646 | 53.1 | 52.1 |
| Southern Highlands High Thermal Inertia and Spectrally Distinct Materials: PSP_010326_1560 PSP_010471_1560 (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 | -23.7 | 44.9 | 4.00 | 18.94 | 67.2 | 65.4 |
| Phyllosilicates in Acidalia Region: PSP_009538_2220 PSP_010039_2220 (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 | 41.78 | 309. | 0.48 | 17.37 | 44.8 | 46.8 |
| Medusae Fossae Formation and Cratered Cemented Dunes: PSP_009609_1675 PSP_010453_1675 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.5 | 178. | 5.31 | -18.9 | 62.4 | 62.6 |
| Cluster of Craters and Edifices on Top of Mesa: PSP_009642_2215 PSP_010143_2215 (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 | 41.10 | 350. | -1.2 | 16.64 | 45.5 | 47.8 |
| 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 |
| A North Polar Crater: PSP_009689_2645 PSP_010084_2645 (Interval in Earth days: 31) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.33 | 120. | -1.7 | 12.07 | 62.3 | 65.3 |
| Swirls of Rock in Candor Chasma: PSP_001984_1735 PSP_001918_1735 (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 | -6.47 | 283. | -0.7 | 22.04 | 56.8 | 55.1 |
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