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.
| Intact Stratigraphy in Crater Central Peak in Thaumasia Planum: ESP_018044_1540 ESP_018466_1540 (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 | -25.7 | 295. | -3.9 | -17.4 | 71.1 | 71.3 |
| Exposure of Polar Layered Deposits: ESP_018096_2710 ESP_018071_2690 (Interval in Earth days: 2) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 88.99 | 190. | -17. | -17.5 | 64.8 | 64.3 |
| Terrain East of Hellas Planitia: ESP_017854_1470 ESP_018487_1470 (Interval in Earth days: 50) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -32.6 | 83.0 | 0 | -19.3 | 75.9 | 76.2 |
| Lava in Olympus Mons Aureole: ESP_018033_2045 ESP_018323_2045 (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 | 24.47 | 228. | 3.37 | 27.97 | 43.6 | 42.2 |
| Very Well-Preserved 10-Kilometer Diameter Impact Crater: ESP_017901_2375 ESP_017980_2375 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 57.35 | 225. | 8.89 | 25.25 | 44.9 | 43.6 |
| Well-Preserved Oblique Impact Crater in Acidalia Planitia: ESP_017792_2285 ESP_018425_2285 (Interval in Earth days: 50) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 47.90 | 323. | 9.53 | -4.67 | 42.0 | 45.6 |
| Rampart Crater Sample: ESP_018010_2455 ESP_018656_2455 (Interval in Earth days: 51) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 65.42 | 128. | 2.96 | 17.4 | 49.0 | 51.6 |
| Exposure of Polar Layered Deposits: ESP_018043_2715 ESP_018084_2685 (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 | 88.51 | 196. | -13. | -12.9 | 64.5 | 63.9 |
| Valley-Crater Intersection with Exposed Layers: ESP_018055_2120 ESP_018899_2120 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 31.60 | 346. | 3.16 | -20.2 | 42.5 | 48.6 |
| Clay Diversity on Flank of Mawrth Vallis: ESP_017897_2045 ESP_018530_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 | 24.08 | 341. | 4.44 | -14.5 | 43.4 | 46.8 |
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