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.
| Gemina Lingula Scarp with Outcrop of Layered Deposits and Unconformities: ESP_018778_2605 ESP_018897_2605 (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 | 80.23 | 26.7 | 6.03 | -9.11 | 61.6 | 63.8 |
| Layered Terrain in Aeolis Planum: ESP_018603_1755 ESP_019592_1755 (Interval in Earth days: 77) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.68 | 150. | 5.39 | -11.1 | 56.5 | 56.6 |
| Fractures in North Polar Layered Deposits: ESP_018760_2650 ESP_018825_2650 (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 | 85.03 | 138. | 5.15 | 18.36 | 64.7 | 65.3 |
| Impact Crater Exposing Bedrock in Thaumasia Planum: ESP_018611_1565 ESP_019323_1565 (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 | -23.4 | 294. | -3.4 | 8.81 | 68.5 | 64.3 |
| Youthful Crater on Northern Plains: ESP_018712_2395 ESP_019147_2395 (Interval in Earth days: 34) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 59.35 | 44.4 | 4.26 | 22.15 | 50.5 | 53.8 |
| Interior Wall and Ejecta of 20-Kilometer Diameter Crater near Toro Crater: ESP_018553_1975 ESP_019265_1975 (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 | 17.27 | 73.0 | -0.7 | 11.33 | 47.3 | 49.0 |
| Flow-Like Mound in Equatorial Crater: ESP_018542_1715 ESP_019254_1715 (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 | -8.57 | 16.1 | 4.25 | 17.12 | 58.9 | 56.5 |
| Central Pit of an Impact Crater: ESP_018703_1570 ESP_019204_1570 (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 | -22.6 | 303. | -7.7 | 11.51 | 67.9 | 64.3 |
| Crosscutting Relationships between Persbo Crater Ejecta and Viscous Flows: ESP_018550_1890 ESP_019262_1890 (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 | 8.989 | 156. | -8.3 | 4.302 | 50.9 | 51.2 |
| Light-Toned Layered Rock in Ridge in Coprates Chasma: ESP_018545_1670 ESP_019824_1670 (Interval in Earth days: 100) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.9 | 294. | 1.64 | 20.31 | 61.7 | 56.2 |
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