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.
| Possible MSL Landing Site in Gale Crater: ESP_018854_1755 ESP_018920_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 | -4.58 | 137. | 5.54 | -18.0 | 56.2 | 57.8 |
| Pits North of Alba Patera: ESP_018955_2310 ESP_018256_2310 (Interval in Earth days: 54) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 50.63 | 254. | -14. | 11.85 | 51.4 | 43.8 |
| Well-Preserved Crater Northeast of Hellas Planitia: ESP_019120_1585 ESP_027678_1585 (Interval in Earth days: 667) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -21.2 | 77.3 | 3.42 | -7.57 | 64.5 | 65.6 |
| Cerberus Fossae near Head of Athabasca Valles: ESP_018985_1900 ESP_019618_1900 (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 | 9.954 | 157. | 17.7 | -2.49 | 49.1 | 52.8 |
| Steep North Polar Boundary Scarp: ESP_018928_2640 ESP_019034_2640 (Interval in Earth days: 8) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.79 | 237. | 7.24 | -7.09 | 65.4 | 67.3 |
| Abrupt Transition in Expression of North Polar Basal Stratigraphy: ESP_018898_2645 ESP_019215_2645 (Interval in Earth days: 24) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.25 | 342. | 0 | -13.9 | 65.7 | 70.4 |
| Possible Fluvial Features in West Hellas Planitia: ESP_019042_1450 ESP_019187_1450 (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 | -34.8 | 48.5 | 4.88 | 17.60 | 73.2 | 71.3 |
| Thermally-Distinct Material at Distal Coogoon Valles: ESP_019084_1980 ESP_060437_1980 (Interval in Earth days: 3222) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.85 | 336. | -5.5 | 5.547 | 49.5 | 37.7 |
| Central Structure of Jorn Crater: ESP_019186_1525 ESP_025199_1525 (Interval in Earth days: 469) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -27.1 | 76.4 | 0 | -29.5 | 67.8 | 62.4 |
| North Polar Trough Stratigraphy: ESP_019102_2660 ESP_018496_2660 (Interval in Earth days: 47) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 85.86 | 179. | -12. | -22.1 | 69.8 | 64.4 |
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