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.
| 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 |
| Gullies, Ridges and Thrust Faults Are in This Region: PSP_002068_1510 PSP_002912_1510 (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 | -28.7 | 152. | -1.5 | -26.0 | 65.3 | 59.4 |
| 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 |
| 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 |
| Schiaparelli Crater Sedimentary Layers: PSP_002218_1800 PSP_002930_1800 (Interval in Earth days: 55) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -0.09 | 14.4 | -8.1 | 10.03 | 55.8 | 55.0 |
| Sublimation Process / Spider Development : PSP_003075_0930 PSP_003062_0930 (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 | -87.0 | 86.6 | -0.3 | -2.01 | 80.7 | 81.1 |
| Chasma Boreale: PSP_001386_2650 PSP_009193_2650 (Interval in Earth days: 608) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.93 | 2.32 | 0.09 | -21.1 | 67.5 | 61.5 |
| Fretted Terrain Valleys and Apron Materials: PSP_001334_2215 PSP_001466_2215 (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 | 40.95 | 12.0 | 5.55 | -3.77 | 48.0 | 49.9 |
| Zumba Crater: Fresh Crater with Impressive Ejecta/Ray Pattern: PSP_002118_1510 PSP_003608_1510 (Interval in Earth days: 116) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -28.6 | 226. | 6.73 | 23.47 | 64.3 | 47.3 |
| 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 |
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