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.
| Layers and Spider Terrain : ESP_048726_1020 ESP_048990_1020 (Interval in Earth days: 20) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -77.9 | 23.5 | 6.68 | -14.2 | 57.4 | 60.1 |
| Deeply Incised Gullies and Arcuate Ridges : ESP_048926_1355 ESP_048992_1355 (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 | -44.3 | 312. | 7.06 | -10.7 | 36.0 | 37.3 |
| Light-Toned Deposits in Rypin Crater : ESP_048886_1785 ESP_048820_1785 (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 | -1.28 | 319. | 2.91 | 25.36 | 39.9 | 39.1 |
| Galap Crater Gullies : ESP_048693_1420 ESP_048983_1420 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.6 | 192. | 5.84 | 27.48 | 34.6 | 31.6 |
| Pit in Mantle Deposit : ESP_048947_1260 ESP_049013_1260 (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 | -53.7 | 101. | -3.8 | -18.1 | 41.8 | 43.0 |
| Gully Monitoring : ESP_048733_1410 ESP_049023_1410 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.7 | 182. | -5.9 | 18.04 | 35.5 | 32.8 |
| Terraced Crater in Southern Mid-Latitudes : ESP_048762_1335 ESP_048907_1335 (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 | -46.3 | 111. | -7.4 | 3.141 | 38.2 | 37.3 |
| Possible Flow Material at Bakhuysen Crater Rim : ESP_048950_1575 ESP_049095_1575 (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 | -22.4 | 14.6 | 0.32 | 15.89 | 32.0 | 29.9 |
| Spider Morphology Off South Polar Layered Deposits : ESP_048650_1000 ESP_048808_1000 (Interval in Earth days: 12) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -79.8 | 304. | -0.5 | 13.38 | 59.2 | 58.8 |
| Diverse Terrain for Seasonal Action : ESP_048857_0990 ESP_040444_0990 (Interval in Earth days: 656) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -81.0 | 58.4 | -8.2 | 8.058 | 61.4 | 64.4 |
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