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.
| Oudemans Crater Central Peak: PSP_008340_1700 ESP_026273_1700 (Interval in Earth days: 1397) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.83 | 268. | 0 | 29.10 | 57.8 | 55.8 |
| Dome-Shaped Feature: PSP_008828_1665 PSP_009606_1665 (Interval in Earth days: 61) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -13.2 | 262. | 1.26 | -19.9 | 62.3 | 64.5 |
| Flows on the Northeastern Flank of Arsia Mons: PSP_008565_1720 PSP_009844_1720 (Interval in Earth days: 100) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.68 | 242. | 9.15 | -10.2 | 57.2 | 60.4 |
| Light-Toned Outcrops in Noctis Labyrinthus: PSP_009118_1665 ESP_028080_1665 (Interval in Earth days: 1478) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -13.4 | 263. | 5.47 | -16.3 | 62.9 | 60.4 |
| Crater Floor and Central Mound in Gale Crater (MSL): PSP_009650_1755 PSP_009716_1755 (Interval in Earth days: 5) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.61 | 137. | 10.8 | -12.4 | 57.4 | 59.0 |
| Valleys Cut in Bedrock: PSP_009082_1605 ESP_053665_1605 (Interval in Earth days: 3474) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -19.1 | 166. | 5.29 | -7.86 | 66.6 | 64.3 |
| Defrosting Dunes: PSP_009122_2600 PSP_009439_2600 (Interval in Earth days: 25) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 79.97 | 122. | 14.9 | -10.0 | 56.0 | 58.6 |
| Key Contact Relationships and Morphologic Correlations: PSP_009279_2650 PSP_009451_2650 (Interval in Earth days: 13) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.69 | 156. | -5.6 | -19.3 | 60.6 | 62.2 |
| Cross-Cutting Fractures in the Utopia Region: PSP_008280_2190 PSP_009005_2190 (Interval in Earth days: 57) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.89 | 101. | -7.4 | 7.203 | 42.3 | 42.0 |
| Textured Plain in Arcadia Planitia: PSP_008566_2285 ESP_016069_2285 (Interval in Earth days: 585) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 48.18 | 209. | -4.0 | -26.0 | 43.4 | 49.7 |
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