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.
| Capri Chasma: ESP_027564_1655 ESP_053818_1655 (Interval in Earth days: 2046) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -14.5 | 308. | -4.4 | 5.774 | 61.8 | 60.3 |
| Complex Superposition of Fractures: ESP_027486_2240 ESP_027631_2240 (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 | 43.43 | 269. | -1.1 | 13.86 | 45.3 | 45.2 |
| Small Crater on North Polar Layered Deposits: ESP_027548_2635 ESP_027443_2635 (Interval in Earth days: 9) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.46 | 346. | 6.21 | -8.50 | 63.1 | 62.9 |
| Field of Shallow Depressions: ESP_027581_2185 ESP_028504_2185 (Interval in Earth days: 72) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.22 | 197. | -3.7 | 29.11 | 45.6 | 52.4 |
| Linear Ridges: ESP_027229_1825 ESP_028350_1825 (Interval in Earth days: 87) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.474 | 89.8 | 7.62 | -4.36 | 51.7 | 53.4 |
| Depression in CTX P13_006195_1728_XN_07S202W and THEMIS V14574001: ESP_027398_1740 ESP_027886_1740 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.87 | 157. | 6.23 | -7.42 | 56.3 | 56.6 |
| Ridges Radial To Wall of Crater: ESP_027072_1620 ESP_035221_1620 (Interval in Earth days: 635) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -17.9 | 59.5 | -6.6 | 11.48 | 64.9 | 64.2 |
| Phyllosilicate Deposits of Possible Hydrothermal Origins in Exhumed Terrain: ESP_027270_1530 ESP_027758_1530 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -26.4 | 55.0 | -1.9 | -16.6 | 70.1 | 69.1 |
| Crater with Layered Material in THEMIS Image V18397010: ESP_027100_1990 ESP_028643_1990 (Interval in Earth days: 120) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 18.61 | 10.2 | -2.1 | -14.8 | 45.5 | 54.4 |
| Dune Migration: ESP_027341_2580 ESP_027578_2580 (Interval in Earth days: 19) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 77.65 | 256. | -4.2 | 17.63 | 58.2 | 58.9 |
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