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.
| Margin of Smooth Lobate Deposit in Nereidum Montes: ESP_086259_1405 ESP_085824_1405 (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 | -39.1 | 321. | -1.8 | -16.3 | 61.6 | 55.3 |
| Mesa Stratigraphy at Terby Crater: ESP_086268_1525 ESP_086835_1525 (Interval in Earth days: 44) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -27.1 | 73.7 | 3.54 | -8.39 | 53.5 | 62.3 |
| Layers in Crater in Northeast Sinus Meridiani: ESP_086244_1805 ESP_086666_1805 (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 | 0.362 | 5.66 | 2.87 | -23.9 | 40.6 | 46.6 |
| Hillslope Morphologies Southeast of Ostrov Crater: ESP_086219_1520 ESP_085375_1520 (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 | -27.5 | 332. | -6.1 | 8.78 | 53.6 | 40.3 |
| Possible Thin Glacial Lobe in Young Crater: ESP_086309_1490 ESP_086810_1490 (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 | -30.4 | 35.6 | -7.9 | 3.638 | 56.9 | 63.4 |
| A Slice through the Layercake: ESP_084979_1975 ESP_085045_1975 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.49 | 336. | 16.6 | -4.34 | 44.6 | 45.3 |
| Transverse Dunes West of Argyre Planitia: ESP_085825_1300 ESP_085759_1300 (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 | -49.8 | 294. | -2.2 | 12.44 | 61.9 | 59.9 |
| Possible Esker in Phlegra Montes: ESP_085948_2165 ESP_086673_2165 (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 | 36.15 | 164. | -8.9 | 24.11 | 48.0 | 41.2 |
| Giant Polygon Terminus: ESP_085849_2205 ESP_086996_2205 (Interval in Earth days: 90) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 39.92 | 346. | 2.02 | 17.45 | 50.4 | 42.0 |
| Diverse Materials in Western Jezero Crater Rim: ESP_085714_1985 ESP_085859_1985 (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 | 18.41 | 77.2 | -23. | -5.54 | 42.3 | 40.4 |
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