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.
| North Flank of Apollinaris Patera: PSP_001645_1725 PSP_002634_1725 (Interval in Earth days: 77) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.40 | 174. | 4.03 | 29.14 | 57.3 | 53.4 |
| Layering in North Polar Layered Deposits (Lower Correlated Sequence): PSP_001640_2640 PSP_001652_2640 (Interval in Earth days: 1) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.79 | 276. | 2.44 | 27.03 | 69.9 | 69.5 |
| Dissected Wall of Mojave Crater: PSP_001481_1875 PSP_002167_1880 (Interval in Earth days: 54) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 7.783 | 326. | 3.49 | -17.4 | 51.7 | 55.6 |
| Northern Plains Sample: PSP_001945_2515 PSP_002077_2515 (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 | 71.07 | 252. | 2.20 | -10.6 | 67.3 | 70.4 |
| Boulder Tracks with Boulders at Ends: PSP_001730_1740 PSP_002086_1740 (Interval in Earth days: 27) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.87 | 16.4 | -2.4 | 21.5 | 57.0 | 54.7 |
| White Rock Deposits: PSP_002033_1720 PSP_002099_1720 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.01 | 25.0 | 5.96 | -17.5 | 56.7 | 58.4 |
| Chasma Boreale Scarp with Possible Gypsum: PSP_001374_2650 PSP_001518_2650 (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 | 85.02 | 338. | -7.1 | 13.56 | 67.8 | 68.9 |
| Lineated Valley Fill in Coloe Fossae : PSP_002902_2205 PSP_003245_2205 (Interval in Earth days: 27) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 40.17 | 53.8 | 3.42 | -28.6 | 68.0 | 74.6 |
| Dark Gullies in Western Argyre Region: PSP_002023_1275 PSP_002102_1275 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -51.9 | 304. | -0.5 | 24.14 | 78.1 | 75.4 |
| Gullies Possibly Produced by Snow/Ice Melting: PSP_002023_2320 PSP_002524_2320 (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 | 51.75 | 288. | 8.79 | 22.34 | 59.2 | 66.1 |
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