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 Alcove Within the Arsia Mons Southwest Rift Zone: PSP_009910_1690 PSP_010543_1690 (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 | -10.7 | 239. | 17.3 | -3.84 | 60.3 | 60.4 |
| 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 |
| 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 |
| 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 |
| 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 |
| Graben in Memnonia Fossae: PSP_010346_1570 PSP_010491_1570 (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 | -23.0 | 219. | -5.8 | 9.284 | 67.3 | 65.6 |
| High-Latitude Exposure of North Polar Layered Deposits: PSP_010069_2680 PSP_010479_2680 (Interval in Earth days: 32) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.94 | 145. | -8.3 | -15.7 | 68.7 | 73.9 |
| Rayed Crater on Southeast Flank of Elysium Mons: PSP_009333_2025 PSP_009834_2025 (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 | 22.46 | 151. | -21. | -0.87 | 47.7 | 47.8 |
| Central Pit of Large But Well-Preserved Crater: PSP_009585_1660 PSP_010429_1660 (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 | -13.7 | 113. | 5.01 | -19.0 | 63.2 | 63.2 |
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