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.
Crater Rim and Ejecta in Olympus Mons Aureole: ESP_017295_2050 ESP_017440_2050 (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 | 24.54 | 218. | -3.9 | 8.729 | 42.5 | 41.8 |
Eastern Portion of Well-Preserved 10-Kilometer Diameter Impact Crater: ESP_017101_1810 ESP_017312_1810 (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 | 0.766 | 116. | 7.04 | -2.87 | 50.2 | 52.0 |
Diverse Lava Morphologies in Elysium Planitia: ESP_017271_1870 ESP_017416_1870 (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 | 6.820 | 155. | -6.6 | 7.712 | 48.9 | 48.5 |
Nili Patera: ESP_016905_1890 ESP_035181_1890 (Interval in Earth days: 1424) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 8.910 | 67.6 | 0 | 17.66 | 45.7 | 47.4 |
Central Structure and Layered Bedrock in 25-Kilometer Diameter Crater: ESP_017002_1535 ESP_017147_1535 (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 | -26.0 | 303. | -3.1 | 10.15 | 67.4 | 67.7 |
Exposure of Lower Layers in South Melas Chasma with Stratigraphic Contacts: ESP_016963_1680 ESP_018598_1680 (Interval in Earth days: 127) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.1 | 286. | -0.9 | 16.30 | 57.5 | 60.1 |
Possible Olivine-Rich Terrain: ESP_016903_1820 ESP_018248_1820 (Interval in Earth days: 105) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 1.941 | 123. | 0.64 | -15.9 | 48.8 | 54.5 |
Filled Crater in Amazonis Planitia at End of Marte Vallis: ESP_017032_2050 ESP_018100_2050 (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 | 24.66 | 198. | -5.6 | 7.91 | 42.0 | 43.4 |
Light-Toned Mounds in Acidalia Planitia: ESP_017132_2250 ESP_017633_2250 (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 | 44.43 | 345. | -6.6 | 5.659 | 42.7 | 41.6 |
Exposure of North Polar Layered Deposits: ESP_017106_2670 ESP_071530_2670 (Interval in Earth days: 4240) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.18 | 267. | 0 | -6.89 | 64.3 | 65.6 |
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