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.
Central Peak with Layered Bedrock: PSP_005683_1640 ESP_011458_1640 (Interval in Earth days: 450) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -15.7 | 96.8 | 5.59 | 18.89 | 32.6 | 57.3 |
Pair of Odd Craters of Hrad Vallis Deposit: PSP_006881_2145 PSP_010375_2145 (Interval in Earth days: 272) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 34.25 | 141. | 6.74 | -8.95 | 42.8 | 51.5 |
Large Crater on South Polar Layered Deposits: PSP_005695_1015 PSP_005603_1015 (Interval in Earth days: 7) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -78.2 | 146. | -0.6 | -21.2 | 69.9 | 69.8 |
Sulfates in Ius Chasma: PSP_006652_1725 ESP_023398_1725 (Interval in Earth days: 1305) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.47 | 279. | 0 | 14.79 | 39.1 | 30.7 |
Light-Toned Layering along Plains Adjacent to Melas Chasma: PSP_005030_1685 ESP_012427_1685 (Interval in Earth days: 576) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -11.2 | 284. | 3.48 | -15.1 | 35.7 | 53.6 |
Oblique Impact Exposing Bedrock within A Libya Montes Massif: PSP_005934_1845 ESP_013766_1845 (Interval in Earth days: 611) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 4.265 | 81.9 | 4.88 | 28.69 | 35.1 | 42.8 |
Basal Exposure of South Polar Layered Deposits: PSP_005089_1040 PSP_005313_1040 (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 | -75.8 | 131. | -6.9 | 7.077 | 60.1 | 61.9 |
Mound in Utopia Plains: PSP_005973_2200 ESP_011471_2200 (Interval in Earth days: 429) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 39.48 | 93.2 | -4.4 | 24.72 | 55.5 | 63.8 |
Distal Ramparts of Chryse Planitia Crater: PSP_006677_2000 ESP_023423_2000 (Interval in Earth days: 1305) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 19.72 | 313. | -2.7 | 10.75 | 38.9 | 42.2 |
Faded Ray from Tomini Crater and Hebrus Valles Streamlined Islands: PSP_006552_2000 PSP_007343_2000 (Interval in Earth days: 62) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 19.64 | 126. | 0 | 24.05 | 38.9 | 37.5 |
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