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.
| On the Shape of Impact Craters: ESP_044998_1745 ESP_046409_1745 (Interval in Earth days: 110) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.41 | 271. | 0 | -14.4 | 54.1 | 53.0 |
| Bedrock Exposures on the Floor of Bakhuysen Crater: ESP_044981_1560 ESP_051785_1560 (Interval in Earth days: 530) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -23.6 | 16.0 | 20.2 | -3.50 | 64.6 | 58.9 |
| Highly Disrupted Crater in Elysium Planitia : ESP_045319_1830 ESP_051147_1830 (Interval in Earth days: 454) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.984 | 148. | 5.22 | 26.84 | 48.8 | 34.9 |
| Sinuous Ridges in Aeolis Region : ESP_045121_1740 ESP_052637_1740 (Interval in Earth days: 586) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.99 | 153. | 7.90 | -17.7 | 53.6 | 54.9 |
| Tilted Blocks of Layered Bedrock : ESP_045343_1930 ESP_046200_1930 (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 | 12.83 | 212. | -3.0 | 19.15 | 45.8 | 47.7 |
| High-Latitude Exposure of North Polar Layered Deposits : ESP_045251_2720 ESP_045223_2720 (Interval in Earth days: 2) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 88.16 | 87.4 | -8.4 | -18.6 | 69.0 | 70.1 |
| Dune Monitoring : ESP_045334_2580 ESP_044675_2580 (Interval in Earth days: 51) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 77.96 | 83.9 | -6.1 | -28.7 | 61.5 | 58.2 |
| Valley with Central Ridge in Southwest Utopia Planitia : ESP_045163_2165 ESP_045308_2165 (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 | 36.02 | 82.8 | -4.1 | 14.93 | 42.7 | 41.9 |
| North Polar Gypsum Dunes : ESP_045263_2605 ESP_045500_2605 (Interval in Earth days: 18) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 80.40 | 213. | 4.05 | 18.68 | 61.7 | 63.6 |
| Chain of Collapse Pits Near Olympica Fossae : ESP_045302_2035 ESP_050906_2035 (Interval in Earth days: 437) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 23.36 | 249. | 6.09 | -19.1 | 42.8 | 38.4 |
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