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.
| Bedrock Stratigraphy Exposed in Crater Wall: ESP_026333_2015 ESP_026478_2015 (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 | 21.35 | 68.7 | 0.94 | 15.99 | 42.4 | 41.5 |
| Dunes and North Polar Outlier in CTX P21_009399_2597_XN_79N230W: ESP_026554_2590 ESP_026462_2590 (Interval in Earth days: 7) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 78.92 | 131. | 13.3 | -2.45 | 55.1 | 56.0 |
| Fresh 3-Kilometer Crater in Tyrrhena Terra: ESP_026253_1680 ESP_027387_1680 (Interval in Earth days: 88) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -11.8 | 97.7 | -8.2 | 17.03 | 59.5 | 59.1 |
| Well-Preserved Impact Crater: ESP_026238_1520 ESP_053692_1525 (Interval in Earth days: 2140) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -27.9 | 149. | -6.6 | 13.05 | 70.5 | 69.2 |
| Cratered Cones in Cydonia Region: ESP_026204_2175 ESP_034762_2175 (Interval in Earth days: 667) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 37.24 | 348. | 1.69 | -26.7 | 40.0 | 43.5 |
| Heavily Dissected Ancient Bedrock: ESP_026319_1740 ESP_062846_1740 (Interval in Earth days: 2846) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.17 | 94.7 | -3.5 | -16.0 | 55.9 | 58.6 |
| Leveed Channel Near Impact Crater: ESP_026235_2320 ESP_026525_2320 (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 | 51.84 | 220. | -6.1 | 12.06 | 43.3 | 41.8 |
| Syrtis Major Terrain Sample: ESP_026280_1975 ESP_027902_1975 (Interval in Earth days: 126) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.50 | 76.7 | -5.6 | 6.391 | 44.0 | 47.8 |
| Well-Exposed Bedrock Layers in Northern Hellas Planitia: ESP_026492_1540 ESP_036052_1540 (Interval in Earth days: 745) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -25.9 | 54.4 | -4.8 | 7.826 | 70.0 | 70.5 |
| Central Peak of Crater in Syrtis Major: ESP_026386_1825 ESP_027586_1825 (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 | 2.280 | 64.8 | -6.7 | 3.498 | 51.4 | 52.3 |
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