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.
| Gullies in Southern Hemisphere Crater: ESP_013894_1410 ESP_022676_1410 (Interval in Earth days: 684) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.8 | 195. | -5.6 | 5.235 | 37.6 | 35.2 |
| Crater in the Sirenum Fossae Region: ESP_012918_1450 ESP_013340_1450 (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 | -34.4 | 201. | -7.6 | -20.0 | 44.4 | 40.3 |
| South Polar Layered Deposits Exposed in Bend in Trough Wall: ESP_013830_0940 ESP_014027_0940 (Interval in Earth days: 15) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.7 | 172. | 7.85 | 26.64 | 66.5 | 67.5 |
| Exposure of Thick Layered Deposits in Hebes Chasma: ESP_013205_1790 ESP_021565_1790 (Interval in Earth days: 651) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -0.82 | 283. | -25. | -3.43 | 50.5 | 51.4 |
| Eastern Tooting Crater Impact Processes: ESP_013735_2035 ESP_014157_2035 (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 | 23.18 | 207. | 6.42 | -8.32 | 57.4 | 52.6 |
| Well-Preserved 12 Kilometer Impact Crater on East Rim in Isidis Region: ESP_014016_1945 ESP_022376_1945 (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 | 14.52 | 98.4 | -8.6 | 14.23 | 48.5 | 51.5 |
| Dry Falls in the Southern Branch of Kasei Valles: ESP_013152_1980 ESP_013297_1980 (Interval in Earth days: 11) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.90 | 285. | 3.51 | 15.70 | 60.2 | 58.1 |
| Layering on Floor of Noctis Labyrinthus Pit: ESP_014076_1680 ESP_021513_1680 (Interval in Earth days: 579) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -11.8 | 263. | -5.4 | 13.21 | 35.2 | 46.5 |
| Landslides at the Edge of the South Polar Layered Deposits: ESP_013026_1080 ESP_013224_1080 (Interval in Earth days: 15) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -71.9 | 143. | -8.2 | -28.8 | 56.2 | 56.7 |
| Comparative Gully Morphology: ESP_013934_1335 ESP_014000_1335 (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 | -46.0 | 183. | 6.35 | -11.3 | 40.0 | 41.5 |
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