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.
| 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 |
| Impact Crater on North Polar Layered Deposits: PSP_001612_2670 PSP_001956_2670 (Interval in Earth days: 26) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 86.85 | 290. | 0.48 | -11.1 | 72.0 | 77.4 |
| Scalloped Terrain: PSP_001331_2260 PSP_002162_2260 (Interval in Earth days: 64) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 45.62 | 93.6 | 0 | 19.66 | 49.2 | 58.0 |
| Mantling Material Exposed on Plateau Cut by Cliff Face : PSP_002413_1410 PSP_002492_1410 (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 | -38.4 | 95.1 | -0.8 | 29.23 | 66.4 | 63.1 |
| Layering in North Polar Layered Deposits (Lower Correlated Sequence): PSP_001640_2640 PSP_001652_2640 (Interval in Earth days: 1) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.79 | 276. | 2.44 | 27.03 | 69.9 | 69.5 |
| Layers on Floor of West Candor Chasma: PSP_002195_1745 PSP_002406_1745 (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 | -5.19 | 282. | -5.3 | -11.5 | 56.6 | 56.9 |
| 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 |
| Athabasca Valles Distributary Channel: PSP_001540_1890 PSP_002371_1890 (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 | 8.783 | 155. | 16.5 | -3.96 | 50.4 | 55.2 |
| Boulder Tracks with Boulders at Ends: PSP_001730_1740 PSP_002086_1740 (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 | -5.87 | 16.4 | -2.4 | 21.5 | 57.0 | 54.7 |
| Fresh-Looking Gullies: PSP_001714_2390 PSP_001846_2390 (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 | 58.73 | 82.3 | 3.50 | -8.24 | 57.8 | 60.7 |
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