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.
| Mesa Stratigraphy at Terby Crater: ESP_083486_1530 ESP_083697_1530 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -26.9 | 73.5 | -4.8 | -22.6 | 44.7 | 43.5 |
| Leveed Feature on North-Facing Valles Marineris Wall Landslide or Glacier: ESP_083425_1710 ESP_084282_1710 (Interval in Earth days: 67) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.95 | 295. | 7.89 | -17.7 | 48.8 | 40.7 |
| Troughs Overlying South Polar Layered Deposit: ESP_083661_0930 ESP_083871_0930 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.0 | 23.7 | 6.04 | 20.10 | 64.9 | 63.6 |
| Fissure South of Ascraeus Mons: ESP_083321_1780 ESP_083598_1780 (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 | -2.07 | 253. | 1.71 | -24.3 | 53.1 | 52.2 |
| West Hellespontus Complex Dune Field: ESP_083342_1395 ESP_083909_1395 (Interval in Earth days: 44) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -40.1 | 45.1 | 7.14 | -8.63 | 46.1 | 40.8 |
| Landslide on Crater Wall: ESP_083410_1935 ESP_083344_1935 (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 | 13.28 | 341. | 7.82 | 25.40 | 60.0 | 59.1 |
| Alluvial Fan Features in Nereidum Montes: ESP_083543_1450 ESP_083754_1450 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -34.5 | 317. | 2.41 | -21.0 | 43.2 | 42.5 |
| Linear Ridges Intersecting Valley Topography: ESP_083580_1530 ESP_083514_1530 (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 | -26.5 | 28.7 | -23. | 0.494 | 45.0 | 43.9 |
| Diverse Periglacial Terrain: ESP_083337_1410 ESP_083759_1410 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.8 | 181. | 5.38 | -15.7 | 46.0 | 42.4 |
| Hillslope Morphologies Southeast of Ostrov Crater: ESP_083371_1520 ESP_083516_1520 (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 | -27.5 | 332. | -4.5 | 17.35 | 46.1 | 42.5 |
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