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.
The Edge of Olympus Mons: PSP_005019_1970 PSP_005441_1970 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.02 | 221. | 2.77 | -13.5 | 51.3 | 46.9 |
Geologic Contacts Near Ganges Chasma: PSP_005082_1700 ESP_011991_1700 (Interval in Earth days: 538) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.68 | 305. | -2.8 | 14.87 | 36.1 | 54.7 |
South Polar Layered Deposits: PSP_005011_0885 PSP_005023_0915 (Interval in Earth days: 1) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -88.4 | 191. | 16.5 | 16.24 | 69.4 | 68.8 |
Ridges East of the Nectaris Fossae: PSP_003948_1540 PSP_004370_1540 (Interval in Earth days: 32) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -25.6 | 306. | 0.21 | -12.1 | 44.8 | 40.5 |
Gullies and Mantling Material: PSP_004113_1425 PSP_005036_1425 (Interval in Earth days: 72) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.1 | 123. | -5.9 | 7.401 | 43.2 | 35.4 |
Low Shield with Radial Flows East of the Olympica Fossae: PSP_003818_2040 PSP_004108_2040 (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 | 23.71 | 249. | -3.0 | 23.54 | 65.9 | 63.5 |
Sublimation Process / Spider Evolution: PSP_003312_0930 PSP_003325_0930 (Interval in Earth days: 1) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -86.9 | 91.3 | 1.36 | 3.43 | 76.2 | 75.8 |
Layers Exposed in the Central Uplift of an Unnamed Crater: PSP_003803_1515 ESP_013679_1515 (Interval in Earth days: 770) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -28.3 | 304. | 5.29 | -11.0 | 46.2 | 36.5 |
Glacial-Like Fractures in Proposed Glacial Ice in Arsia Mons Depression: PSP_004201_1735 PSP_005256_1735 (Interval in Earth days: 83) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.62 | 236. | 8.32 | -25.5 | 46.4 | 37.5 |
Geologic Contact Between Wallrock and Light-Toned Layered Deposits: PSP_004344_1715 PSP_005623_1715 (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 | -8.25 | 293. | -3.3 | 15.97 | 44.9 | 32.1 |
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