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.
| Eroding Margin of Low Latitude North Polar Layered Deposits: PSP_009938_2640 PSP_010176_2640 (Interval in Earth days: 19) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.87 | 139. | 19.6 | 5.57 | 63.3 | 66.3 |
| Basal Unit and Dunes: PSP_009913_2635 PSP_010019_2635 (Interval in Earth days: 9) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.51 | 118. | 8.64 | -5.81 | 63.1 | 64.9 |
| Unconformity in Gemina Lingula Layered Deposits: PSP_010088_2610 PSP_010827_2610 (Interval in Earth days: 58) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 80.70 | 32.6 | 6.60 | -18.7 | 63.2 | 75.4 |
| Stratigraphy of Potential Crater Hydrothermal System: PSP_010228_1490 ESP_016320_1490 (Interval in Earth days: 475) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -30.6 | 202. | -7.4 | 12.70 | 72.4 | 62.4 |
| Sapping Features East of Tooting Crater: PSP_010333_2025 PSP_010689_2025 (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 | 22.14 | 208. | -3.9 | 0.754 | 50.8 | 53.1 |
| Gullies in North Mid-Latitude Crater: PSP_009744_2305 PSP_010245_2305 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 50.11 | 84.3 | -0.6 | 14.78 | 47.4 | 50.9 |
| Mounds in Ulysses Fossae: PSP_009409_1860 PSP_009554_1860 (Interval in Earth days: 11) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 5.804 | 237. | -7.2 | 8.646 | 53.1 | 52.1 |
| High-Latitude Exposure of North Polar Layered Deposits: PSP_010146_2680 PSP_010623_2680 (Interval in Earth days: 37) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.86 | 180. | -6.3 | -17.5 | 69.8 | 76.1 |
| Ends of Two Polar Troughs: PSP_010040_2640 PSP_010290_2640 (Interval in Earth days: 20) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.78 | 264. | -6.7 | 8.656 | 65.3 | 67.5 |
| Basal Unit and North Polar Layered Deposits in Chasma Boreale Scarp: PSP_009995_2650 PSP_010128_2650 (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 | 85.06 | 0.70 | 19.4 | 5.177 | 65.3 | 66.6 |
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