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.
| Ganges Chasma Landslide: ESP_024333_1715 ESP_025401_1715 (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 | -8.34 | 315. | -6.9 | 14.61 | 38.8 | 49.6 |
| Valley Termini on Western Hecates Tholus: ESP_024418_2125 ESP_024273_2125 (Interval in Earth days: 12) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 32.42 | 149. | 1.81 | -15.4 | 41.6 | 43.8 |
| Rocky Outcrops Northwest of Elysium Region: ESP_024537_2080 ESP_072314_2080 (Interval in Earth days: 3723) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 27.64 | 140. | 2.98 | 22.18 | 39.0 | 50.8 |
| Channel in Lava Flow: ESP_024530_1570 ESP_042200_1570 (Interval in Earth days: 1377) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -22.6 | 338. | -5.9 | 11.68 | 48.5 | 49.2 |
| Degraded Crater East of Argyre Planitia: ESP_024372_1305 ESP_033299_1305 (Interval in Earth days: 696) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -49.3 | 335. | -0.0 | 25.62 | 64.2 | 65.0 |
| Syrtis Major Planum Plains: ESP_024513_1980 ESP_025370_1980 (Interval in Earth days: 67) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 18.01 | 76.8 | 4.69 | 27.70 | 36.4 | 37.2 |
| Possible Kaolinite Mound Deposits on Kashira Crater Floor: ESP_024464_1525 ESP_024965_1525 (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 | -27.2 | 341. | -4.2 | 9.459 | 50.2 | 56.8 |
| Dunes: ESP_024542_1870 ESP_024608_1870 (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 | 7.077 | 6.74 | 1.72 | -21.7 | 36.4 | 38.9 |
| Possible Phyllosilicates in Southern Argyre Planitia: ESP_024386_1235 ESP_085798_1235 (Interval in Earth days: 4785) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -56.1 | 314. | 7.85 | -7.17 | 69.3 | 66.3 |
| Material on Crater Floor West of Flammarion Crater: ESP_024435_2045 ESP_028391_2045 (Interval in Earth days: 308) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.44 | 46.5 | -3.9 | 10.17 | 38.7 | 50.5 |
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