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.
| North Polar Dune Changes: ESP_026872_2580 ESP_026819_2580 (Interval in Earth days: 4) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 77.63 | 97.5 | 2.01 | 16.24 | 55.3 | 54.3 |
| Landslide on North Wall of Montevallo Crater in THEMIS V26773021: ESP_026654_1955 ESP_027643_1955 (Interval in Earth days: 77) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 15.54 | 305. | 3.72 | 19.19 | 45.1 | 46.2 |
| Pits and Channels in Amazonis Planitia: ESP_026605_2025 ESP_051290_2025 (Interval in Earth days: 1924) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 22.23 | 202. | 3.69 | 14.57 | 42.6 | 35.3 |
| Flows and Trough in Western Lycus Sulci Region: ESP_026908_2065 ESP_028662_2065 (Interval in Earth days: 136) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 26.16 | 210. | -1.8 | -16.0 | 42.9 | 55.6 |
| Southwestern Acidalia Planitia: ESP_026772_2170 ESP_028394_2170 (Interval in Earth days: 126) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 36.50 | 321. | 3.40 | 21.61 | 40.9 | 51.3 |
| Curving Exposure of North Polar Layered Deposits: ESP_026662_2625 ESP_027058_2625 (Interval in Earth days: 30) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 82.53 | 58.6 | 4.44 | -9.71 | 58.0 | 59.8 |
| Ripple Changes in Trough: ESP_026831_1910 ESP_028031_1910 (Interval in Earth days: 93) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 10.65 | 156. | -20. | 4.382 | 49.4 | 49.9 |
| Dunes and North Polar Outlier in MOC Image R23-00720: ESP_026607_2590 ESP_026910_2590 (Interval in Earth days: 24) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 78.95 | 131. | -0.7 | 14.42 | 55.9 | 55.6 |
| Channel Source Area South of Ascraeus Mons: ESP_026867_1820 ESP_027223_1820 (Interval in Earth days: 27) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.009 | 253. | -6.6 | 12.03 | 52.6 | 51.7 |
| Cones at Edge of North Polar Layered Deposits: ESP_026694_2605 ESP_026602_2605 (Interval in Earth days: 7) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 80.44 | 268. | 7.91 | -6.06 | 56.4 | 57.1 |
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