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.
Active Geyser Locale: ESP_014083_0945 ESP_014122_0945 (Interval in Earth days: 3) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.4 | 103. | 8.28 | 22.35 | 69.3 | 68.8 |
Impact Crater with a Rocky Central Uplift: ESP_012947_1735 ESP_022441_1735 (Interval in Earth days: 740) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.55 | 125. | 4.88 | 27.14 | 48.6 | 37.0 |
Possible Cyclic Bedding in Arabia Terra: ESP_013611_1910 ESP_014033_1910 (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 | 10.87 | 355. | 0.61 | -17.2 | 50.8 | 46.6 |
Exposure of Polar Layered Deposits Not Well Observed: ESP_013886_0875 ESP_022748_0875 (Interval in Earth days: 691) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.4 | 165. | 4.63 | 10.95 | 71.0 | 71.9 |
Central Uplift of Well-Exposed Taytay Crater : ESP_012794_1875 ESP_012939_1875 (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 | 7.398 | 340. | 8.24 | 23.49 | 56.4 | 54.2 |
Central Pit Gullies in Asimov Crater: ESP_013123_1330 ESP_013268_1330 (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 | -46.8 | 4.93 | 13.8 | 22.63 | 42.3 | 40.3 |
Rocky Deposit on Crater Floor with Thermal Signature: ESP_012788_1365 ESP_013856_1365 (Interval in Earth days: 84) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -43.2 | 151. | 2.54 | 20.66 | 46.5 | 37.4 |
Graben Wall with Gullies: ESP_013736_1415 ESP_013947_1415 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.1 | 188. | 1.89 | -6.61 | 36.9 | 37.5 |
Basal Exposure of South Polar Layered Deposits: ESP_013857_1070 ESP_014015_1070 (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 | -72.6 | 135. | -5.1 | 19.52 | 57.3 | 57.5 |
Well-Preserved Gullied Impact Crater: ESP_012925_1220 ESP_013202_1220 (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 | -57.6 | 13.0 | 7.46 | -9.50 | 48.8 | 47.4 |
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