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.
Well-Preserved Impact Crater: ESP_022365_2190 ESP_030989_2190 (Interval in Earth days: 672) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.64 | 37.1 | -3.5 | -17.5 | 70.9 | 73.5 |
Mounds in Northern Chryse Region and Possible MSL Rover Landing Site: ESP_022526_2140 ESP_022592_2140 (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 | 33.86 | 321. | 2.25 | -14.1 | 64.9 | 64.9 |
Layered Material in Crater Seen in CTX Image: ESP_022425_1925 ESP_058609_1925 (Interval in Earth days: 2820) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 12.54 | 202. | -5.4 | 8.895 | 50.6 | 37.5 |
Uplift of Layered Materials From the Intersection of Two Craters: ESP_022580_1560 ESP_023213_1560 (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 | -23.6 | 294. | 2.93 | -18.0 | 32.9 | 33.9 |
Inca City Ice-Free: ESP_022699_0985 ESP_022607_0985 (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 | -81.4 | 295. | 21.7 | 6.9 | 62.5 | 62.4 |
Light-Toned Layered Sediments Exposed within Pit at Noctis Labyrinthus: ESP_022436_1705 ESP_022502_1705 (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 | -9.45 | 263. | 16.5 | -6.37 | 36.6 | 37.5 |
Wrinkle Ridges in West Meridiani Planum: ESP_022657_1775 ESP_023369_1775 (Interval in Earth days: 56) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -2.49 | 350. | 0.52 | 20.48 | 38.4 | 31.2 |
Arkhangelsky Crater Dunes: ESP_022605_1390 ESP_023106_1390 (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 | -40.7 | 335. | -0.6 | 16.18 | 36.3 | 37.7 |
Central Pit of 45-Kilometer Diameter Crater in Tyrrhena Terra: ESP_022614_1635 ESP_023458_1635 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -16.1 | 85.4 | 8.64 | -19.9 | 33.2 | 33.9 |
Arsia Mons Reticulate Bedform Change Detection: ESP_022661_1705 ESP_022938_1705 (Interval in Earth days: 21) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.17 | 239. | 28.3 | -7.66 | 33.4 | 33.6 |
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