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.
Well-Preserved Large Crater Near Tempe Terra: ESP_016251_2045 ESP_016396_2045 (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 | 24.34 | 280. | 1.79 | 16.28 | 39.6 | 38.6 |
Juventae Chasma: ESP_016145_1775 ESP_017424_1775 (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 | -2.49 | 298. | -12. | 7.841 | 45.5 | 53.7 |
Lineated Valley Fill Near Deuteronilus Region: ESP_016168_2180 ESP_024594_2180 (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 | 37.78 | 23.8 | 4.56 | -7.15 | 42.2 | 43.8 |
Gullied Crater: ESP_016263_2310 ESP_016553_2310 (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 | 50.59 | 308. | 3.22 | 21.47 | 47.2 | 43.9 |
Sinuous Ridges in the Aeolis and Zephyria Regions: ESP_016282_1750 ESP_016915_1750 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.04 | 155. | 22.5 | 8.613 | 45.4 | 52.2 |
Massif with Radial Troughs in Viking 072A02: ESP_016011_2185 ESP_016499_2185 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.06 | 347. | 25.6 | 2.429 | 41.2 | 41.5 |
Yardang-Forming Material in Crater in THEMIS V14074003: ESP_016268_1675 ESP_016901_1675 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.5 | 180. | 8.02 | -6.63 | 50.4 | 57.6 |
Well Exposed Deep Bedrock in Northern Hellas Basin: ESP_015903_1505 ESP_016536_1505 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -29.4 | 68.1 | -3.8 | -20.0 | 56.7 | 66.2 |
Lobate Landform North of Reull Vallis: ESP_016047_1410 ESP_020293_1410 (Interval in Earth days: 331) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.6 | 97.2 | 4.47 | -12.9 | 64.7 | 63.9 |
Well-Preserved 3-Kilometer Diameter Gullied Crater: ESP_016002_2285 ESP_016134_2285 (Interval in Earth days: 10) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 47.99 | 234. | 1.86 | -24.6 | 47.8 | 49.0 |
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