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.
| Crater Floor and Central Mound in Gale Crater (MSL): PSP_009650_1755 PSP_009716_1755 (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 | -4.61 | 137. | 10.8 | -12.4 | 57.4 | 59.0 |
| Pits along the Claritas Rupes: PSP_008512_1630 PSP_009013_1630 (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 | -16.6 | 251. | 6.29 | -8.58 | 62.9 | 65.6 |
| Flows on the Northeastern Flank of Arsia Mons: PSP_008565_1720 PSP_009844_1720 (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 | -7.68 | 242. | 9.15 | -10.2 | 57.2 | 60.4 |
| High-Latitude Exposure of North Polar Layered Deposits: PSP_009190_2680 PSP_009350_2680 (Interval in Earth days: 13) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.89 | 0.19 | -6.5 | -13.7 | 63.4 | 63.4 |
| Outcrop of Light-Toned Deposit South of Coprates Chasma: PSP_009143_1645 ESP_052737_1645 (Interval in Earth days: 3397) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -15.1 | 301. | -4.2 | 13.31 | 64.6 | 59.4 |
| Central Peak of Large Well-Preserved Crater: PSP_008860_2165 ESP_053799_2160 (Interval in Earth days: 3502) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 35.93 | 101. | 5.76 | -5.62 | 41.8 | 42.8 |
| Abrading Dome Dunes in the North Polar Erg: PSP_009295_2565 PSP_009743_2565 (Interval in Earth days: 35) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 76.17 | 95.3 | -6.2 | 15.45 | 55.6 | 56.7 |
| Characterize Surface Hazards and Science of Possible MSL Rover Landing Site: PSP_008469_2040 PSP_008825_2040 (Interval in Earth days: 28) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 23.95 | 340. | 3.44 | -15.0 | 42.8 | 45.4 |
| High-Latitude Exposure of North Polar Layered Deposits: PSP_009280_2675 PSP_009426_2675 (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 | 87.50 | 105. | -8.5 | -18.0 | 62.8 | 63.6 |
| Key Contact Relationships and Morphologic Correlations: PSP_009279_2650 PSP_009451_2650 (Interval in Earth days: 13) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.69 | 156. | -5.6 | -19.3 | 60.6 | 62.2 |
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