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.
| Candidate Recent Impact Site: ESP_065360_1900 ESP_065703_1900 (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 | 10.06 | 217. | -7.7 | -26.7 | 61.5 | 61.7 |
| Sinuous Channel Form on South Rim of Baldet Crater: ESP_065339_2015 ESP_066236_2015 (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 | 21.43 | 65.7 | 24.4 | 12.89 | 64.7 | 62.1 |
| Gullied Slope: ESP_065466_1455 ESP_065809_1455 (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 | -34.1 | 209. | -3.7 | -19.0 | 50.3 | 47.1 |
| Possible Phyllosilicate-Rich Terrain in Nirgal Vallis and Gully Monitoring: ESP_065330_1505 ESP_065752_1505 (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 | -29.0 | 320. | -8.0 | 15.14 | 52.1 | 45.2 |
| Gullies with Terminal Ridges in Terra Cimmeria: ESP_065323_1330 ESP_065732_1330 (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 | -46.4 | 153. | -0.8 | -27.4 | 53.8 | 50.3 |
| Flow-Like Feature in Chryse Planitia: ESP_065356_1995 ESP_065422_1995 (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 | 19.37 | 323. | 5.19 | -11.2 | 65.1 | 66.3 |
| USGS Dune Database Entry 2579-573: ESP_065438_1225 ESP_065517_1225 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -57.3 | 257. | -4.7 | 21.47 | 55.7 | 52.7 |
| Layering in Wall of Orson Welles Crater: ESP_065396_1800 ESP_073600_1800 (Interval in Earth days: 639) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -0.16 | 315. | -2.7 | 8.009 | 56.8 | 56.9 |
| Gullied Slope: ESP_065493_1415 ESP_065427_1415 (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 | -38.3 | 193. | -8.5 | 6.271 | 50.6 | 50.4 |
| Flat Layered Deposits and Candidate Exit Breach in Small Young Crater: ESP_065414_1495 ESP_065480_1495 (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 | -30.3 | 186. | 8.30 | -7.95 | 49.9 | 50.3 |
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