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.
| Small Fan in Amenthes Fossae Region: ESP_019264_1895 ESP_019897_1895 (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 | 9.201 | 101. | 5.29 | -10.3 | 51.1 | 54.7 |
| Rim and Ejecta of Very Fresh 7-Kilometer Diameter Crater in Arcadia Region: ESP_019547_2335 ESP_024848_2335 (Interval in Earth days: 413) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 53.29 | 288. | 5.88 | -21.5 | 58.3 | 51.5 |
| Well-Preserved 6-Kilometer Diameter Impact Crater: ESP_019371_1700 ESP_020571_1700 (Interval in Earth days: 94) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.81 | 63.1 | 4.37 | -11.4 | 57.7 | 55.3 |
| Claritas Fossae Region with Possible Serpentine: ESP_019509_1530 ESP_019654_1530 (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 | -26.8 | 258. | -8.0 | 9.024 | 66.0 | 63.8 |
| Lava Vent with Channels: ESP_019325_1960 ESP_019391_1960 (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 | 15.69 | 235. | 7.19 | -14.6 | 49.9 | 52.1 |
| Diverse Lithologies in Central Uplift of Stokes Crater: ESP_019380_2360 ESP_019604_2360 (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 | 55.59 | 171. | -16. | 10.82 | 58.7 | 59.7 |
| Crater in Sinus Sabaeus Region: ESP_019386_1700 ESP_020019_1700 (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 | -10.0 | 13.6 | 3.93 | -10.0 | 57.8 | 57.1 |
| Alpine Glacier: ESP_019213_2210 ESP_019503_2210 (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 | 40.86 | 51.3 | -8.0 | 14.46 | 51.2 | 52.7 |
| Northern Plains Crater with Summer Ice: ESP_018809_2495 ESP_019033_2495 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 69.28 | 273. | -1.9 | 13.56 | 56.4 | 57.8 |
| North Polar Layered Deposit Basal Stratigraphy: ESP_018945_2645 ESP_019564_2645 (Interval in Earth days: 48) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.42 | 138. | 0 | 15.70 | 66.4 | 74.4 |
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