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.
| Gullies in Recent Impact Crater in Terra Sirenum: PSP_005586_1425 PSP_005731_1425 (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 | -37.4 | 228. | -4.2 | 9.845 | 39.4 | 40.1 |
| Exposure of South Polar Layered Deposits and Residual Cap: PSP_005466_0950 PSP_005571_0950 (Interval in Earth days: 8) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -84.8 | 298. | -0.9 | 13.27 | 72.2 | 72.7 |
| Xanthe Terra Crater: PSP_006598_1780 ESP_033326_1780 (Interval in Earth days: 2083) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -2.16 | 313. | 2.29 | 24.68 | 37.1 | 37.0 |
| Unnamed Well-Preserved Crater in Cimmeria Terra: PSP_005286_1480 PSP_005576_1480 (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 | -31.5 | 140. | -27. | -1.66 | 36.8 | 36.4 |
| Chains of Cones in Isidis Planitia: PSP_006725_1945 PSP_006936_1945 (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 | 14.23 | 83.0 | 8.28 | -4.15 | 36.9 | 38.5 |
| Landforms in Athabasca Valles: PSP_006696_1895 PSP_007408_1895 (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 | 9.346 | 155. | 3.28 | -6.76 | 36.8 | 42.0 |
| Survey South Polar Layered Deposits: PSP_004593_0830 PSP_004984_0970 (Interval in Earth days: 30) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -82.6 | 140. | 0 | -19.2 | 72.1 | 65.8 |
| Spallanzani Crater - Swirl Patterns in Lower Layers along Northern Margin: PSP_005565_1220 PSP_005842_1220 (Interval in Earth days: 21) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -57.7 | 86.3 | -5.0 | -20.8 | 52.1 | 57.2 |
| Seasonal Monitoring: PSP_005553_0980 PSP_005790_0980 (Interval in Earth days: 18) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -82.1 | 75.6 | -8.4 | 8.644 | 71.5 | 74.2 |
| Lineated Valley Flow and Dissected Mantle Terrain in Chaotic Region: PSP_006807_2185 PSP_007097_2185 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.22 | 2.06 | -3.1 | 14.00 | 46.0 | 42.9 |
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