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.
| Fan-Shaped Deposit with Floor Outcrop in Camichel Crater: ESP_064750_1825 ESP_065304_1825 (Interval in Earth days: 43) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.468 | 308. | 4.35 | -28.4 | 57.9 | 60.2 |
| Well-Exposed Crater Ejecta in Tyrrhena Terra: ESP_064877_1670 ESP_064811_1670 (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 | -12.9 | 83.0 | 8.74 | 27.89 | 55.5 | 54.1 |
| Flow-Like Feature within Chryse Planitia: ESP_064868_2005 ESP_064156_2005 (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 | 20.24 | 324. | 13.0 | -11.5 | 62.9 | 58.6 |
| Eroded Crater near Lowell Crater: ESP_064711_1325 ESP_065265_1325 (Interval in Earth days: 43) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -47.1 | 300. | -0.9 | -26.2 | 63.2 | 56.9 |
| Landform in CTX Image G03_019466_2032_XN_23N014W: ESP_064709_2035 ESP_072979_2035 (Interval in Earth days: 644) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 23.38 | 345. | -4.9 | 6.945 | 64.2 | 58.2 |
| Ares Vallis: ESP_064670_1945 ESP_064815_1945 (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 | 14.30 | 331. | -1.9 | 16.18 | 60.8 | 60.2 |
| Valleys in Crater Northeast of Argyre Planitia: ESP_064736_1500 ESP_064591_1500 (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 | -29.7 | 335. | 0.30 | -16.8 | 58.2 | 61.0 |
| Fractures in Chryse Planitia: ESP_064855_2000 ESP_065765_2000 (Interval in Earth days: 70) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 19.68 | 320. | -3.6 | 8.387 | 63.9 | 64.4 |
| Nicholson Crater: ESP_064530_1800 ESP_064807_1800 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 0.058 | 195. | -0.4 | -23.4 | 57.6 | 59.8 |
| Flow-Like Feature within Chryse Planitia: ESP_064723_2000 ESP_072993_2000 (Interval in Earth days: 644) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 19.95 | 324. | -6.0 | 5.877 | 63.2 | 57.9 |
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