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.
Stratigraphy Exposed in Ius Chasma: PSP_007430_1725 PSP_009645_1725 (Interval in Earth days: 173) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.24 | 276. | -2.2 | -22.0 | 48.2 | 61.2 |
Eroded Sediments in West Candor Chasma: PSP_009460_1745 ESP_017741_1745 (Interval in Earth days: 645) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.49 | 284. | 18.2 | 6.762 | 57.4 | 56.6 |
Translucent Ice in North Polar Region: PSP_009696_2575 PSP_009736_2575 (Interval in Earth days: 3) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 77.49 | 300. | 8.01 | -18.2 | 57.6 | 59.8 |
Unnamed, Well-Preserved Crater South of Hypanis Valles: PSP_009393_1890 PSP_010105_1890 (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 | 8.973 | 313. | -3.9 | 13.87 | 51.3 | 51.3 |
Water Bearing Minerals in Noctis Labyrinthus: PSP_009474_1705 PSP_010107_1705 (Interval in Earth days: 50) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.28 | 263. | -0.3 | -20.5 | 60.9 | 61.8 |
Dark Spot Near Olmpus Mons Volcano: PSP_009502_1980 ESP_015950_1980 (Interval in Earth days: 503) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.62 | 216. | -2.0 | 26.27 | 48.1 | 36.5 |
Stratigraphic Relationships West of Tenuis Cavus: PSP_009166_2650 PSP_009760_2650 (Interval in Earth days: 47) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 85.01 | 355. | -1.8 | -15.7 | 60.3 | 64.1 |
High-Latitude Exposure of North Polar Layered Deposits: PSP_009187_2680 ESP_018221_2680 (Interval in Earth days: 704) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.92 | 95.3 | -6.5 | -14.0 | 63.1 | 63.7 |
Near the Head of Lethe Vallis: PSP_009056_1840 PSP_009900_1840 (Interval in Earth days: 65) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 3.802 | 153. | 6.66 | -22.9 | 52.4 | 55.9 |
Exposure of Polar Layered Deposits Not Well Observed by Previous Missions: PSP_009039_2680 PSP_009133_2680 (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 | 88.00 | 169. | -8.0 | -15.3 | 63.1 | 63.0 |
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