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.
| Remnant of Unusual Looking Material on Plains: ESP_012675_1565 ESP_013743_1565 (Interval in Earth days: 83) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -23.0 | 353. | -1.3 | 22.39 | 47.7 | 33.5 |
| Circular Features: ESP_013460_1095 ESP_013302_1095 (Interval in Earth days: 13) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -70.4 | 165. | 26.6 | 0.477 | 51.6 | 53.3 |
| Valley with Central Ridge Located North of Schiaparelli Crater: ESP_014164_1870 ESP_020388_1870 (Interval in Earth days: 485) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 6.827 | 16.4 | 19.0 | -0.77 | 40.3 | 55.8 |
| Well-Preserved 8 Kilometer Diameter Crater: ESP_013650_1230 ESP_013927_1230 (Interval in Earth days: 21) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -56.4 | 20.2 | 1.13 | -19.3 | 45.0 | 47.6 |
| Martian Volcanic Vent with Elevated Rim: ESP_013008_1825 ESP_020801_1825 (Interval in Earth days: 607) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.452 | 259. | -3.3 | 21.93 | 52.7 | 53.7 |
| Exposures of Layered Bedrock Northwest of Hellas Basin: ESP_012620_1540 ESP_013688_1540 (Interval in Earth days: 84) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -25.5 | 55.4 | 3.80 | 26.88 | 47.8 | 33.4 |
| Differential Erosion of Light-Toned Stratigraphy in Melas Chasma: ESP_013640_1710 ESP_012928_1710 (Interval in Earth days: 56) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.93 | 285. | 8.51 | -10.3 | 39.1 | 48.9 |
| Pit Crater: ESP_013167_1785 ESP_013589_1785 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -1.32 | 239. | -7.4 | -22.9 | 49.4 | 45.4 |
| Phyllosilicate and Possible Chlorite Prehnite Northwest of Hellas Region: ESP_012765_1535 ESP_013477_1535 (Interval in Earth days: 55) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -26.2 | 56.4 | 7.51 | 22.87 | 45.6 | 35.6 |
| Basal Exposure of South Polar Layered Deposits: ESP_013290_1075 ESP_013092_1075 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -72.2 | 138. | -18. | 5.428 | 55.8 | 55.0 |
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