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.
| Light Toned Ridges in Meridiani Region: PSP_003682_1805 PSP_003972_1805 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 0.329 | 5.15 | -0.2 | 29.79 | 54.2 | 50.0 |
| Channel Flow: PSP_003978_1715 PSP_004334_1715 (Interval in Earth days: 28) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.28 | 205. | -3.3 | 7.629 | 48.8 | 44.2 |
| Light-Toned Deposit in Tithonium Chasma: PSP_003514_1755 PSP_005848_1755 (Interval in Earth days: 182) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.60 | 271. | 6.07 | -6.81 | 52.9 | 34.2 |
| Layered Sinuous Ridge in Argyre Planitia: PSP_003816_1245 PSP_004106_1245 (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 | -55.1 | 314. | 3.82 | 21.86 | 51.2 | 46.0 |
| Gully Previously Identified in MOC Image M08-00012: PSP_003842_1245 PSP_005319_1245 (Interval in Earth days: 115) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -55.2 | 324. | 1.51 | -26.3 | 51.0 | 48.7 |
| Mangala Source: PSP_003635_1615 PSP_005613_1615 (Interval in Earth days: 154) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -18.2 | 210. | -1.4 | -22.8 | 49.5 | 34.9 |
| Stratigraphic Section Through Aram Chaos: PSP_003406_1830 PSP_003683_1830 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.909 | 339. | 7.38 | -22.2 | 55.5 | 56.9 |
| Breached Impact Crater in Elysium Planitia: PSP_004151_1810 ESP_020963_1810 (Interval in Earth days: 1310) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 0.869 | 160. | 1.37 | -21.1 | 50.9 | 56.5 |
| Gullies in Southern Latitude Crater: PSP_004145_1455 ESP_013098_1455 (Interval in Earth days: 698) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -34.3 | 329. | -0.1 | -21.4 | 42.1 | 43.2 |
| South Polar Layered Deposit Comparison with Higher Latitude Scarps: PSP_003868_0940 PSP_003896_0940 (Interval in Earth days: 3) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.7 | 13.2 | -0.6 | -19.9 | 67.4 | 70.0 |
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