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.
Light-Toned Material along Valley near Coprates Catena: ESP_022527_1645 ESP_023028_1645 (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 | -15.5 | 300. | 1.62 | 23.37 | 34.6 | 29.7 |
Eastern Half of Iazu Crater: ESP_022670_1775 ESP_023092_1775 (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 | -2.69 | 354. | 8.00 | -9.77 | 37.6 | 34.9 |
Stratigraphy of Kasimov Crater Fill: ESP_022473_1550 ESP_023119_1550 (Interval in Earth days: 50) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -24.9 | 337. | -8.5 | 27.5 | 34.5 | 30.2 |
Mawrth Vallis Strata with Interesting Geometry Exposed in Small Crater: ESP_022354_2035 ESP_022288_2035 (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 | 23.41 | 340. | -8.4 | 11.78 | 59.5 | 59.1 |
Landslides in Valles Marineris: ESP_022632_1670 ESP_031124_1670 (Interval in Earth days: 661) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.6 | 313. | 4.73 | 24.39 | 34.2 | 36.3 |
Lobate Flow Feature in Eastern Hellas: ESP_022494_1385 ESP_022639_1385 (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 | -41.1 | 124. | 5.68 | 20.40 | 36.0 | 34.9 |
Faulted, Layered Deposits in Candor Chasma: ESP_022343_1735 ESP_022699_1735 (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 | -6.63 | 284. | -11. | 0.088 | 40.9 | 36.1 |
Western Rim of Very Well-Preserved Impact Crater: ESP_022291_1995 ESP_022713_1995 (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 | 19.26 | 259. | -3.5 | -14.7 | 56.8 | 52.2 |
Dune Features: ESP_022181_1345 ESP_023025_1345 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -45.1 | 28.8 | 23.5 | 0.924 | 37.4 | 40.5 |
Small Mounds in Chryse Planitia: ESP_022025_2000 ESP_040328_2000 (Interval in Earth days: 1426) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 19.72 | 322. | -4.4 | 12.17 | 59.9 | 52.7 |
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