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.
| Potential Fan Deposit at Head of Mawrth Vallis: ESP_084715_1990 ESP_085005_1990 (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 | 18.91 | 346. | -0.5 | 15.83 | 49.8 | 45.3 |
| Icy Scarp and Gullies: ESP_084723_1250 ESP_084789_1250 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -54.7 | 137. | 6.69 | -10.9 | 47.9 | 49.7 |
| Gullied Crater Wall: ESP_084670_1435 ESP_085593_1435 (Interval in Earth days: 72) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.9 | 142. | 2.83 | 23.40 | 37.7 | 47.0 |
| Hill on South Polar Layered Deposits: ESP_084887_0900 ESP_084374_0900 (Interval in Earth days: 40) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -89.7 | 35.5 | 29.4 | 29.44 | 75.3 | 68.6 |
| Terminus of Fissure in Athabasca Valles: ESP_084867_1900 ESP_085078_1900 (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 | 9.761 | 156. | 0.88 | -9.17 | 42.3 | 41.1 |
| Well-Exposed Bedrock in 3-Kilometer Crater Wall near Oxia Planum: ESP_084755_1975 ESP_085177_1975 (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 | 17.14 | 333. | 6.03 | -14.1 | 47.7 | 44.4 |
| Landforms above Subsurface Radar Observations of South Polar Cap: ESP_084655_1000 ESP_084971_1000 (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 | -80.0 | 208. | -0.0 | 24.15 | 65.9 | 69.1 |
| Well-Preserved 2 to 3-Kilometer Superposed Impact Crater: ESP_084530_1520 ESP_084741_1520 (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 | -27.6 | 4.19 | 6.05 | -21.1 | 34.9 | 37.3 |
| Channel with Streamlined Forms in Northeast Hellas Planitia: ESP_084725_1445 ESP_085635_1445 (Interval in Earth days: 71) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.1 | 80.2 | 0 | -22.7 | 37.9 | 50.3 |
| Fresh Crater: ESP_084505_1405 ESP_085217_1405 (Interval in Earth days: 56) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -39.3 | 328. | 7.64 | -3.64 | 37.9 | 45.2 |
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