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.
| Lighter-Toned Deposits in Young Crater: ESP_085271_1870 ESP_085337_1870 (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 | 7.156 | 287. | -1.6 | -20.0 | 38.2 | 39.4 |
| Channels near Huygens Crater: ESP_085240_1615 ESP_085306_1615 (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 | -18.1 | 57.5 | -4.1 | -22.8 | 36.5 | 38.5 |
| Ice Flow Into Concentric Crater Fill in Nilosyrtis Mensae: ESP_084936_2155 ESP_085292_2155 (Interval in Earth days: 28) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 35.23 | 71.5 | -17. | -6.74 | 59.5 | 54.1 |
| Crater Wall with Potential Chloride Deposit Outcrop: ESP_084905_1470 ESP_085406_1470 (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 | -32.8 | 205. | -5.5 | 26.95 | 38.6 | 42.1 |
| Raised Glacier-Like Forms in Arabia Terra: ESP_085043_2150 ESP_085109_2150 (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 | 34.67 | 27.6 | 6.88 | -10.0 | 56.2 | 56.3 |
| Mesa Stratigraphy at Terby Crater: ESP_085068_1525 ESP_085213_1525 (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 | -27.1 | 74.1 | -4.4 | 13.86 | 37.8 | 37.8 |
| Exposure of South Polar Layered Deposits: ESP_085009_0905 ESP_085037_0905 (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 | -89.5 | 289. | 29.6 | 26.87 | 77.2 | 78.0 |
| Crater in Arabia Terra: ESP_085057_2180 ESP_085202_2180 (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 | 37.41 | 5.91 | -1.0 | 12.91 | 58.5 | 55.8 |
| Fan and Ridges in Southern Gale Crater: ESP_085171_1745 ESP_077088_1745 (Interval in Earth days: 629) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.59 | 137. | 14.5 | -1.72 | 34.1 | 39.5 |
| Phlegra Montes: ESP_085038_2180 ESP_085117_2180 (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 | 37.80 | 164. | -1.4 | 25.59 | 59.1 | 56.4 |
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