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.
| Eastern Rim of Well-Preserved 15-Kilometer Crater Near Alba Mons: ESP_026142_2195 ESP_025852_2195 (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 | 39.10 | 238. | 17.9 | -3.88 | 38.6 | 40.4 |
| Layers of Water-Deposited Sediment: ESP_025665_1825 ESP_026166_1825 (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 | 2.316 | 307. | 2.25 | 28.63 | 46.9 | 47.8 |
| Branching Ridges: ESP_025683_1900 ESP_025538_1900 (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 | 9.786 | 174. | 14.4 | -4.30 | 42.7 | 43.3 |
| Channel in Tharsis Region: ESP_025417_1965 ESP_024916_1965 (Interval in Earth days: 40) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 16.19 | 235. | 17.6 | -8.13 | 38.8 | 38.5 |
| Bedrock Exposed in the Central Uplift of a Unnamed Crater: ESP_025766_2005 ESP_025700_2005 (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 | 20.18 | 69.3 | -7.5 | 11.70 | 41.5 | 39.7 |
| Ridges or Flows in Northeast Gale Crater: ESP_025790_1750 ESP_027135_1750 (Interval in Earth days: 104) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.71 | 137. | -6.0 | 3.949 | 52.2 | 55.9 |
| Depression East-Southeast of Hale Crater and Neighboring Landforms: ESP_025638_1425 ESP_052011_1425 (Interval in Earth days: 2055) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.1 | 330. | -0.2 | -24.4 | 72.7 | 72.5 |
| Abalos Mensa and Abalos Scopuli Region: ESP_025665_2610 ESP_025718_2610 (Interval in Earth days: 4) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 81.01 | 280. | 7.35 | -3.58 | 60.5 | 60.6 |
| Vertically Tilted Blocks of Layers in Becquerel Crater: ESP_025637_2020 ESP_025782_2020 (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 | 21.98 | 351. | -17. | -0.29 | 41.7 | 40.6 |
| Reticulate Bedform Change Detection Northwest Ascraeus Mons: ESP_025667_1960 ESP_026168_1960 (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 | 15.83 | 252. | -8.4 | 18.74 | 42.3 | 42.3 |
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