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.
| Layers in Crater in Protonilus Mensae: ESP_026518_2280 ESP_027863_2280 (Interval in Earth days: 105) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 47.87 | 53.4 | 5.71 | 26.90 | 41.3 | 47.3 |
| Exposure of Nili Fossae Megabreccias: ESP_026346_2000 ESP_026491_2000 (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 | 19.73 | 74.0 | 1.32 | 16.62 | 42.9 | 42.0 |
| Meridiani Planum Terrain Sample: ESP_026283_1810 ESP_026415_1810 (Interval in Earth days: 10) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 1.156 | 354. | 26.9 | -16.8 | 49.2 | 52.9 |
| Eastern Rim of Karzok Crater: ESP_026314_1985 ESP_026670_1985 (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 | 18.39 | 228. | -5.3 | 6.588 | 43.7 | 43.8 |
| Dune Changes in North Polar Crater: ESP_026404_2565 ESP_026457_2565 (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 | 76.14 | 270. | 13.7 | -2.98 | 53.3 | 54.3 |
| Bedrock Stratigraphy Exposed in Crater Wall: ESP_026333_2015 ESP_026478_2015 (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 | 21.35 | 68.7 | 0.94 | 15.99 | 42.4 | 41.5 |
| Olympica Fossae: ESP_026287_2050 ESP_025654_2050 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.58 | 245. | -11. | 3.311 | 42.4 | 39.5 |
| Craters and Mesas in Northeast Arabia Terra: ESP_026254_2085 ESP_026399_2085 (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 | 28.09 | 65.4 | -7.4 | 6.562 | 41.3 | 40.5 |
| Southern Ladon Basin near the Mouth of Ladon Valles: ESP_026139_1600 ESP_027616_1600 (Interval in Earth days: 115) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -19.8 | 329. | 5.17 | -12.8 | 63.6 | 65.3 |
| How Did Valles Marineris Form?: ESP_025415_1675 ESP_026259_1675 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.3 | 294. | 0 | -17.9 | 53.1 | 60.5 |
Page 591 of 896 (8,955 images) | |||||