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.
Cratered Cones on Zephyria Planum: PSP_008832_1770 PSP_009478_1770 (Interval in Earth days: 51) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -3.08 | 152. | -6.8 | 18.94 | 56.5 | 55.9 |
Volcano at Confluence of Samara and Ladon Valles: PSP_008812_1655 PSP_009023_1655 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -14.3 | 338. | 9.90 | -10.8 | 62.4 | 64.3 |
Gullies: PSP_008984_2135 ESP_017476_2135 (Interval in Earth days: 662) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 33.30 | 315. | 3.85 | -10.4 | 42.5 | 42.3 |
Oudemans Crater Central Peak: PSP_008340_1700 ESP_026273_1700 (Interval in Earth days: 1397) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.83 | 268. | 0 | 29.10 | 57.8 | 55.8 |
Olivine-Rich Deposits Off of the Ladon Impact Basin: PSP_009234_1675 PSP_009656_1675 (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 | -12.5 | 336. | -0.6 | -16.3 | 62.8 | 63.8 |
Light-Toned Outcrops in Noctis Labyrinthus: PSP_009118_1665 ESP_028080_1665 (Interval in Earth days: 1478) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -13.4 | 263. | 5.47 | -16.3 | 62.9 | 60.4 |
Polar Layered Deposits Unconformity: PSP_009241_2630 PSP_009637_2630 (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 | 82.84 | 109. | 7.77 | -6.45 | 58.6 | 61.2 |
Seasonal Frost on Dunes: PSP_008847_2580 PSP_009256_2580 (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 | 77.98 | 84.0 | -2.5 | -17.7 | 55.7 | 57.3 |
Light-Toned Bedrock with Erosional Channels in Eos Chasma: PSP_009169_1670 ESP_016606_1670 (Interval in Earth days: 580) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.6 | 312. | -18. | 3.24 | 63.9 | 54.5 |
Field of Cones in the Tartarus Montes: PSP_008528_2060 PSP_009675_2060 (Interval in Earth days: 90) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 25.80 | 170. | -7.7 | 13.02 | 43.5 | 45.3 |
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