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.
| Thin Smooth Lava Flow in Daedalia Planum: ESP_083335_1535 ESP_061707_1535 (Interval in Earth days: 1685) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -26.0 | 235. | -2.1 | -17.9 | 46.5 | 70.5 |
| Scarp in Hellas Planitia with Linear Gullies: ESP_083473_1315 ESP_083684_1315 (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 | -48.0 | 70.6 | 4.47 | -8.56 | 46.2 | 44.9 |
| Troughs Overlying South Polar Layered Deposit: ESP_083627_0930 ESP_083652_0930 (Interval in Earth days: 2) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.0 | 229. | 7.90 | 29.14 | 64.9 | 63.1 |
| 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 |
| Small Delta or Fan: ESP_083521_1675 ESP_083745_1675 (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 | -12.3 | 196. | -8.2 | 25.62 | 47.7 | 42.4 |
| Troughs Overlying South Polar Layered Deposit: ESP_083648_0935 ESP_083647_0935 (Interval in Earth days: 0) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -86.7 | 11.7 | 7.33 | 24.66 | 64.6 | 63.1 |
| 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 |
| 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 |
| Pyroxene-Rich Materials Surrounding Crater in Northeast Hellas Planitia: ESP_083367_1465 ESP_083789_1465 (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 | -33.3 | 82.0 | 4.33 | -20.4 | 45.4 | 42.1 |
| Troughs Overlying South Polar Layered Deposit: ESP_083662_0915 ESP_083991_0915 (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 | -88.4 | 351. | 20.7 | 24.40 | 64.8 | 64.8 |
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