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.
| Stratigraphic Section Through Aram Chaos: PSP_003406_1830 PSP_003683_1830 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.909 | 339. | 7.38 | -22.2 | 55.5 | 56.9 |
| Geologic Contact Between Wallrock and Light-Toned Layered Deposits: PSP_004344_1715 PSP_005623_1715 (Interval in Earth days: 100) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.25 | 293. | -3.3 | 15.97 | 44.9 | 32.1 |
| Boulders on Lobate Ejecta: PSP_003484_1305 PSP_003563_1305 (Interval in Earth days: 7) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -49.3 | 18.5 | -7.9 | 19.01 | 55.3 | 52.0 |
| Glacial-Like Fractures in Proposed Glacial Ice in Arsia Mons Depression: PSP_004201_1735 PSP_005256_1735 (Interval in Earth days: 83) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.62 | 236. | 8.32 | -25.5 | 46.4 | 37.5 |
| Rotational Landslides or Slumps along the Walls of Bahram Vallis: PSP_003460_2015 PSP_003605_2015 (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 | 21.26 | 303. | -1.0 | 12.74 | 64.0 | 63.4 |
| Multiple Levels of Gullies Seen in MOC Image R11-02000: PSP_004019_1420 PSP_004085_1420 (Interval in Earth days: 5) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.9 | 169. | -0.0 | -19.0 | 44.1 | 44.7 |
| Gullies in Newton Crater: PSP_003675_1375 PSP_005877_1375 (Interval in Earth days: 172) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -42.2 | 201. | 0 | 25.53 | 49.8 | 44.0 |
| Fine Textures Near Headwaters of Warrego Valles: PSP_003633_1385 PSP_004266_1385 (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 | -41.1 | 267. | 5.7 | -9.82 | 49.8 | 42.3 |
| Layered Deposit in Crommlin Crater: PSP_003432_1850 PSP_005766_1850 (Interval in Earth days: 182) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 4.980 | 350. | -7.0 | -19.9 | 57.3 | 38.0 |
| Streamlined Form in Kasei Valles: PSP_003408_1990 PSP_003698_1990 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 18.90 | 283. | -4.4 | 23.25 | 62.9 | 61.3 |
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