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.
| Northern Plains West of Erebus Montes: ESP_016650_2205 ESP_035427_2205 (Interval in Earth days: 1464) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 40.26 | 185. | -1.2 | 27.98 | 42.1 | 39.3 |
| Ejecta Flow and Obstacle at Arandas Crater: ESP_016776_2225 ESP_016842_2225 (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 | 42.39 | 344. | 4.98 | -9.79 | 41.8 | 43.0 |
| Dissected Wrinkle Ridge Surrounded by Viscous Flows in Elysium Planitia: ESP_016572_1875 ESP_016150_1875 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 7.515 | 157. | 16.0 | 25.58 | 42.9 | 38.9 |
| Very Large Pit Crater in Daedalia Planum: ESP_016411_1605 ESP_024481_1605 (Interval in Earth days: 629) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -19.4 | 237. | 0 | -21.9 | 56.8 | 47.0 |
| Wallrock Spurs That Are Alligned and Extend Into Melas Chasma: ESP_016528_1705 ESP_016884_1705 (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 | -9.28 | 282. | -8.6 | 5.446 | 52.4 | 54.7 |
| Light-Toned Outcrops in Iani Chaos: ESP_016328_1760 ESP_016473_1760 (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 | -3.82 | 341. | 1.72 | 18.56 | 46.9 | 47.0 |
| Geologic Contact Between Landslides and Blocky Deposit on Floor of Melas Ch: ESP_016739_1715 ESP_018941_1715 (Interval in Earth days: 172) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.58 | 282. | -8.3 | 8.612 | 54.0 | 57.9 |
| Ejecta of Crater Sectioned by Erosion: ESP_016896_1710 ESP_025678_1710 (Interval in Earth days: 684) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.92 | 315. | 6.04 | -5.75 | 54.6 | 53.8 |
| Central Uplift and Olivine-Rich Ponded Material in Elorza Crater: ESP_016659_1710 ESP_017081_1710 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.77 | 304. | 10.5 | -3.93 | 52.2 | 56.4 |
| Crater in Acidalia Planitia: ESP_016841_2340 ESP_017830_2340 (Interval in Earth days: 77) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 53.72 | 7.48 | 5.69 | -6.67 | 45.4 | 44.9 |
Page 701 of 885 (8,850 images) | |||||