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.
10 Kilometer Diameter Rayed Crater: ESP_012738_1785 ESP_013094_1785 (Interval in Earth days: 27) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -1.41 | 70.8 | 2.49 | 14.97 | 53.0 | 48.7 |
Dark Deposits in Gullies in Ariadnes Colles: ESP_013341_1455 ESP_013763_1455 (Interval in Earth days: 32) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -34.3 | 172. | 2.11 | -11.4 | 38.6 | 36.8 |
Gullied Trough Wall: ESP_012602_1415 ESP_013881_1415 (Interval in Earth days: 100) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.3 | 188. | 6.27 | 18.92 | 48.1 | 35.6 |
Gullies and Lobate Material in a Crater in the Nereidum Montes: ESP_014127_1420 ESP_020786_1420 (Interval in Earth days: 519) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.5 | 314. | -2.1 | 19.93 | 37.6 | 54.3 |
Pit on Crater Floor Exposing Layers: ESP_012818_1560 ESP_013174_1560 (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 | -23.8 | 50.3 | -6.3 | 4.629 | 46.1 | 40.7 |
High-Latitude Gullies: ESP_013453_1075 ESP_022789_1075 (Interval in Earth days: 728) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -72.2 | 3.84 | 0.52 | -16.3 | 54.5 | 58.2 |
Differential Erosion of Light-Toned Stratigraphy in Melas Chasma: ESP_013640_1710 ESP_012928_1710 (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 | -8.93 | 285. | 8.51 | -10.3 | 39.1 | 48.9 |
Well Preserved 7-Kilometer Diameter Impact Crater: ESP_012670_1845 ESP_011958_1845 (Interval in Earth days: 55) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 4.679 | 126. | 4.75 | -11.8 | 56.1 | 59.5 |
Exposure of Layered Deposits at End of Bench in Terby Crater: ESP_013516_1520 ESP_013661_1520 (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 | -27.8 | 74.5 | -7.0 | 8.988 | 37.5 | 35.1 |
Basal Exposure of South Polar Layered Deposits: ESP_013290_1075 ESP_013092_1075 (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 | -72.2 | 138. | -18. | 5.428 | 55.8 | 55.0 |
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