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.
| Streamlined Form in Kasei Valles: PSP_003408_1990 PSP_003698_1990 (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 | 18.90 | 283. | -4.4 | 23.25 | 62.9 | 61.3 |
| 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 |
| 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 |
| Gullies Produced by Possible Snow/Ice Melting: PSP_004192_2195 ESP_012446_2195 (Interval in Earth days: 643) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.96 | 116. | -0.0 | 13.62 | 75.3 | 74.8 |
| 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 |
| Loose Cluster of Zunil Crater Secondary Craters: PSP_003874_1815 PSP_004375_1815 (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 | 1.259 | 162. | 4.39 | 27.49 | 53.0 | 47.0 |
| 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 |
| Boulders on Lobate Ejecta: PSP_003484_1305 PSP_003563_1305 (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 | -49.3 | 18.5 | -7.9 | 19.01 | 55.3 | 52.0 |
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