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 |
| Channelized Lava Flow through a Constriction with Well-Preserved Highstands: ESP_018945_2050 ESP_019235_2050 (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 | 24.82 | 171. | -15. | 9.257 | 48.8 | 48.4 |
| 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 |
| 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 |
| Layered Terrains in Aeolis Planum: ESP_018972_1755 ESP_019605_1755 (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 | -4.27 | 154. | 15.7 | -5.86 | 55.1 | 56.0 |
| Cluster of Zunil Crater Secondaries: ESP_019064_1835 ESP_019209_1835 (Interval in Earth days: 12) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 3.656 | 163. | 2.92 | 17.53 | 52.6 | 51.6 |
| 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 |
| Syrtis Major Planum Channel and Depression: ESP_018988_1980 ESP_042882_1980 (Interval in Earth days: 1861) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.54 | 76.5 | 0 | -26.9 | 48.6 | 42.2 |
| Central Chasma Boreale Scarp: ESP_018859_2645 ESP_019043_2645 (Interval in Earth days: 14) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.57 | 343. | -15. | -1.04 | 66.4 | 67.7 |
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