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.
| Very Bright and Sun-Facing Gully Deposits in Hale Crater: ESP_014008_1430 ESP_014153_1430 (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 | -36.4 | 322. | -1.9 | 12.21 | 36.7 | 36.3 |
| Recent Gullies in a Crater in Noachis Terra: ESP_013222_1410 ESP_013288_1410 (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 | -38.8 | 182. | 0.69 | -18.8 | 40.4 | 41.3 |
| Recent Gullies in Well-Preserved Crater: ESP_013667_1345 ESP_013944_1345 (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 | -45.2 | 274. | -4.5 | -28.7 | 40.0 | 42.2 |
| Landforms in Southern Tartarus Colles: ESP_012642_1895 ESP_013710_1895 (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 | 9.266 | 170. | 0.88 | 24.43 | 58.7 | 46.9 |
| Well Preserved 20 Kilometer Diameter Impact Crater: ESP_013684_1455 ESP_020910_1455 (Interval in Earth days: 563) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -34.0 | 168. | -2.8 | 19.71 | 36.4 | 51.7 |
| Basal Exposure of South Polar Layered Deposits: ESP_013857_1070 ESP_014015_1070 (Interval in Earth days: 12) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -72.6 | 135. | -5.1 | 19.52 | 57.3 | 57.5 |
| Central Structure of an Impact Crater in Terra Cimmeria: ESP_013092_1630 ESP_013514_1630 (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 | -16.8 | 129. | -6.4 | -22.9 | 44.0 | 40.3 |
| Layered Bedrock in Northeast Hellas Planitia: ESP_013964_1490 ESP_020267_1490 (Interval in Earth days: 491) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -30.7 | 82.9 | 1.84 | 19.77 | 34.9 | 58.9 |
| Steep Lobate Scarps in Kasei Valles: ESP_012717_1910 ESP_013139_1910 (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 | 10.88 | 282. | 2.07 | -8.93 | 59.1 | 56.6 |
| Light-Toned Layered Material in Trough on North Melas Chasma Wall: ESP_013495_1720 ESP_014128_1720 (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 | -7.82 | 284. | 6.24 | -18.3 | 41.5 | 36.9 |
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