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.
Olivine-Rich Bedrock Exposed in Unnamed Crater Wall in Tyrrhena Terra: PSP_009323_1755 ESP_062992_1755 (Interval in Earth days: 4182) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.60 | 66.3 | -6.2 | 6.454 | 58.4 | 56.3 |
Rayed Thila Crater in Elysium Planitia: PSP_009346_1985 PSP_009491_1985 (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 | 18.08 | 155. | -5.4 | 8.677 | 47.7 | 47.0 |
Pit and Channel on Southwestern Pavonis Mons: PSP_009923_1785 PSP_010213_1785 (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 | -1.67 | 246. | -21. | 14.06 | 58.1 | 55.7 |
Distributaries From Athabasca Valles: PSP_009768_1880 PSP_010045_1880 (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 | 7.721 | 154. | 7.98 | -19.7 | 51.6 | 54.3 |
Exposure of North Polar Layered Deposits for Stratigraphic Analysis: PSP_009951_2670 PSP_010199_2670 (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 | 86.90 | 176. | -17. | 3.468 | 67.0 | 69.6 |
Cones at Edge of North Polar Layered Deposits: PSP_009947_2590 PSP_009710_2590 (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 | 78.66 | 285. | 8.81 | -10.7 | 60.4 | 59.6 |
Fresh or Well-Preserved Chain of Impact Craters in Hesperia Planum: PSP_009572_1620 ESP_016231_1620 (Interval in Earth days: 519) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -17.6 | 109. | -3.3 | 21.86 | 66.2 | 52.1 |
Junction of Three Polar Troughs: PSP_010030_2670 PSP_010532_2670 (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 | 86.74 | 162. | -8.8 | -21.4 | 67.2 | 74.3 |
Polar Layered Deposits Unconformity: PSP_010048_2615 PSP_010509_2615 (Interval in Earth days: 36) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 81.49 | 49.1 | -3.5 | 16.55 | 63.8 | 68.5 |
Potential Paleolake in Crater in Ophir Planum: PSP_010290_1700 PSP_010435_1700 (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 | -10.0 | 306. | 0.86 | 17.82 | 60.3 | 58.8 |
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