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 Delta: ESP_066500_2075 ESP_075640_2075 (Interval in Earth days: 712) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 27.36 | 61.4 | -2.9 | -21.9 | 64.5 | 60.4 |
| Crater Fill Material: ESP_066791_2045 ESP_067411_2045 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.10 | 40.8 | -4.5 | 19.86 | 58.8 | 50.1 |
| Valleys in Crater Northeast of Argyre Planitia: ESP_066886_1500 ESP_067018_1500 (Interval in Earth days: 10) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -29.7 | 334. | 0.58 | -20.8 | 38.1 | 40.1 |
| Subtle Scarp in South Polar Layered Deposits: ESP_066852_0920 ESP_067078_0920 (Interval in Earth days: 18) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.8 | 221. | 18.9 | 8.195 | 69.2 | 73.9 |
| Tilted Strata in Central Structure of Martin Crater: ESP_066848_1585 ESP_067798_1585 (Interval in Earth days: 74) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -21.4 | 290. | -0.1 | -9.63 | 37.8 | 43.4 |
| Slope Streaks in Arabia Terra: ESP_066514_2050 ESP_074889_2050 (Interval in Earth days: 652) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.59 | 40.0 | -5.9 | 9.124 | 62.5 | 64.9 |
| South Polar Layered Deposits: ESP_066784_0915 ESP_067023_0915 (Interval in Earth days: 18) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -88.3 | 284. | 21.7 | 14.13 | 68.7 | 72.9 |
| Gully Topography: ESP_066877_1410 ESP_067154_1410 (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 | -38.8 | 221. | 0.56 | 15.26 | 40.3 | 41.1 |
| Measure Interaction between Wrinkle Ridge and Paleodune Strata: ESP_066818_1865 ESP_073993_1865 (Interval in Earth days: 559) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 6.579 | 25.5 | 4.36 | 22.54 | 46.9 | 57.3 |
| Layered Deposits within Depression in Osuga Valles: ESP_066583_1650 ESP_065897_1650 (Interval in Earth days: 53) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -14.8 | 322. | -10. | 10.02 | 41.2 | 46.6 |
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