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.
| Crater with Gullies, Debris Mantle, Layers Exposed in Eastern Wall: PSP_001948_2140 PSP_002238_2140 (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 | 33.85 | 181. | -3.1 | 20.48 | 54.0 | 55.5 |
| Pristine-Looking Gully : PSP_002692_2295 PSP_002824_2295 (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 | 49.13 | 25.2 | 5.98 | -20.2 | 69.0 | 73.1 |
| North Polar Layered Deposits Exposed Wall: PSP_001488_2665 ESP_019158_2665 (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 | 86.50 | 80.0 | 0.47 | -8.93 | 70.0 | 70.7 |
| Northern Plains Sample: PSP_001945_2515 PSP_002077_2515 (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 | 71.07 | 252. | 2.20 | -10.6 | 67.4 | 70.6 |
| Delta in Crater South of Parana Basin: PSP_001388_1565 PSP_001586_1565 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -23.5 | 347. | -2.1 | -16.1 | 67.0 | 66.9 |
| Field of Morphologically-Diverse Ring/Cone Structures in Athabasca Valles: PSP_001606_1900 PSP_002226_1900 (Interval in Earth days: 48) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 9.645 | 156. | 4.90 | -25.6 | 51.3 | 56.5 |
| Multiple Episodes of Gully Formation, As Seen in MOC Image R16-02071: PSP_002002_1390 PSP_002846_1390 (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 | -40.7 | 155. | 8.34 | -14.7 | 71.6 | 62.7 |
| Layering in Danielson Crater : PSP_002944_1880 ESP_019835_1880 (Interval in Earth days: 1317) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 7.951 | 352. | -11. | 10.60 | 58.1 | 52.8 |
| Small Cones/Mounds in Channel Cutting Secondary Craters of Zunil Crater: PSP_002147_1875 PSP_002292_1875 (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 | 7.388 | 152. | -18. | -3.57 | 55.6 | 54.9 |
| Mawrth Vallis Layered Terrain: PSP_001388_2035 PSP_010183_2035 (Interval in Earth days: 685) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 23.24 | 342. | -5.3 | 8.558 | 48.8 | 48.7 |
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