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.
| Polar Layered Deposit Stratigraphy Near Chasma Australe: PSP_004722_0945 PSP_005052_0945 (Interval in Earth days: 26) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.3 | 94.8 | 0 | -8.15 | 64.7 | 68.1 |
| Basal Exposure of South Polar Layered Deposits: PSP_005458_1035 PSP_005682_1035 (Interval in Earth days: 18) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -76.1 | 134. | 0.86 | 14.88 | 64.4 | 67.1 |
| Gullies Cut into Light-Toned Rock: PSP_006888_1410 ESP_016184_1410 (Interval in Earth days: 724) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.4 | 319. | 2.83 | -23.2 | 59.4 | 68.2 |
| Light-Toned Layered Rock Outcrop in Ladon Vallis: PSP_006637_1590 ESP_023383_1590 (Interval in Earth days: 1305) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -20.8 | 330. | 7.10 | 20.68 | 44.1 | 31.2 |
| Seasonal Monitoring: PSP_005750_0965 PSP_005921_0965 (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 | -83.6 | 99.6 | -2.1 | 13.97 | 75.7 | 77.5 |
| Central Peak with Layered Bedrock: PSP_005683_1640 ESP_011458_1640 (Interval in Earth days: 450) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -15.7 | 96.8 | 5.59 | 18.89 | 32.6 | 57.3 |
| 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 |
| Pair of Odd Craters of Hrad Vallis Deposit: PSP_006881_2145 PSP_010375_2145 (Interval in Earth days: 272) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 34.25 | 141. | 6.74 | -8.95 | 42.8 | 51.5 |
| Gullies in Southern Latitude Crater: PSP_005701_1445 PSP_005991_1445 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.2 | 328. | 0.44 | 26.02 | 39.2 | 41.2 |
| Large Crater on South Polar Layered Deposits: PSP_005695_1015 PSP_005603_1015 (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 | -78.2 | 146. | -0.6 | -21.2 | 69.9 | 69.8 |
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