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.
| High-Latitude Exposure of North Polar Layered Deposits: ESP_028001_2680 ESP_019286_2680 (Interval in Earth days: 679) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.93 | 205. | -13. | -22.6 | 72.3 | 74.2 |
| Fretted Terrain Valley in Viking 084A73 and MOC SP2-45006: ESP_027889_2140 ESP_036394_2140 (Interval in Earth days: 663) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 33.72 | 70.1 | -2.1 | 11.65 | 47.6 | 45.5 |
| Mounds and Small Ridges along Wrinkle Ridge on Huygens Crater Floor: ESP_027969_1635 ESP_028325_1635 (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 | -16.2 | 54.6 | -23. | -4.61 | 62.8 | 60.0 |
| Faults in Claritas Fossae: ESP_028199_1535 ESP_028476_1535 (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 | -26.3 | 254. | 7.56 | -10.8 | 64.9 | 64.2 |
| Extensive Outcrops of Rhythmic Stratigraphy in Arabia Terra: ESP_027918_1905 ESP_027984_1905 (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 | 10.30 | 1.23 | 3.76 | -15.5 | 49.8 | 51.5 |
| Arabia Terra Sample: ESP_027971_1905 ESP_030239_1905 (Interval in Earth days: 176) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 10.17 | 354. | -0.9 | 10.96 | 50.3 | 56.5 |
| Layered Bedrock on Crater Floor: ESP_028074_1605 ESP_028918_1605 (Interval in Earth days: 65) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -19.4 | 66.2 | 4.51 | -9.37 | 62.1 | 58.5 |
| Variable Relief of North Polar Layered Deposits: ESP_028182_2650 ESP_028010_2650 (Interval in Earth days: 13) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.84 | 323. | -3.7 | 8.258 | 72.2 | 69.4 |
| Fan in Crater West of Gale Crater: ESP_027900_1745 ESP_045570_1745 (Interval in Earth days: 1377) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.45 | 136. | -16. | 14.60 | 57.1 | 51.7 |
| Cratered Cones within a Flow Unit in Grjota Valles: ESP_027978_1955 ESP_028466_1955 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 15.18 | 162. | 6.83 | -12.0 | 48.6 | 52.8 |
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