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.
Channels South of the Base of Ascraeus Mons: PSP_001985_1860 PSP_002486_1860 (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 | 5.998 | 254. | -3.9 | 22.18 | 54.0 | 53.5 |
Sample Main Channel of Athabasca Valles : PSP_002938_1890 PSP_003083_1890 (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 | 8.883 | 155. | 4.35 | 20.17 | 57.0 | 56.1 |
Crater and Extensive Field of Secondary Craters Seen in MOC Image R15-02146: PSP_002230_1850 ESP_027890_1850 (Interval in Earth days: 1999) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 4.727 | 46.1 | -7.8 | 4.118 | 55.2 | 51.4 |
Crater/Valley Contact in Licus Vallis : PSP_002082_1755 PSP_002794_1755 (Interval in Earth days: 56) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.21 | 126. | 3.00 | 20.64 | 55.8 | 53.9 |
Possible Phoenix Lander Landing Site: TRA_000881_2475 TRA_000894_2475 (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 | 67.49 | 130. | -21. | 0 | 54.8 | 53.1 |
Positive Relief Features in Parana Basin: PSP_002074_1580 PSP_002786_1580 (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 | -21.9 | 348. | -5.9 | 11.51 | 62.5 | 56.3 |
Dark Crater-Topped Cones in Cydonia Region: PSP_002232_2180 PSP_002377_2180 (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 | 37.56 | 347. | -5.5 | 6.671 | 58.6 | 59.5 |
Interior Channel in Parana Valles: PSP_002008_1560 PSP_002285_1560 (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 | -23.9 | 350. | -0.6 | -27.3 | 63.5 | 63.7 |
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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