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.
| Aram Chaos Mineralogical Variability: PSP_006953_1840 ESP_085467_1840 (Interval in Earth days: 6117) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 3.900 | 339. | 4.39 | -14.5 | 38.8 | 38.0 |
| Sinuous Pits on the Northeast Flank of Ascreaus Mons: PSP_004899_1940 PSP_005387_1935 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 13.58 | 257. | 6.80 | -28.3 | 50.2 | 46.4 |
| Distal Rampart Flow Ejecta of Bacolor Crater: PSP_006750_2130 PSP_007462_2130 (Interval in Earth days: 55) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 32.51 | 118. | 0.23 | -9.07 | 43.2 | 41.8 |
| Wallrock and Plains Contact South of Ius Chasma: PSP_006784_1715 PSP_006929_1715 (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 | -8.35 | 276. | -7.3 | 5.296 | 41.4 | 42.3 |
| Exposure of High-Latitude Polar Layered Deposits Not Well Observed: PSP_005971_0890 PSP_005957_0910 (Interval in Earth days: 1) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -88.7 | 251. | 18.6 | 19.51 | 83.1 | 82.5 |
| Deeply-Penetrating Structure within Polar Layered Deposits: PSP_005076_0940 PSP_005207_0940 (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 | -86.1 | 172. | -8.4 | 5.833 | 69.3 | 69.2 |
| Layering in Northwest-Trending Sinuous Ridge: PSP_006875_1255 ESP_011358_1255 (Interval in Earth days: 349) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -54.0 | 317. | 1.97 | -22.9 | 70.7 | 74.6 |
| Sinuous Features in Light-Toned Material: PSP_006583_1775 PSP_010789_1775 (Interval in Earth days: 328) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -2.28 | 3.05 | 0 | -17.1 | 37.2 | 58.5 |
| Lobate Margin of Impact Ejecta: PSP_006835_2085 PSP_007481_2085 (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 | 28.13 | 319. | -5.9 | 4.424 | 41.5 | 40.0 |
| Valley Network along Melas Chasma Wallrock: PSP_005663_1700 ESP_012493_1700 (Interval in Earth days: 532) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.67 | 282. | -4.4 | -21.3 | 33.4 | 54.0 |
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