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.
| Small Icy Scarp: ESP_079484_2305 ESP_079207_2305 (Interval in Earth days: 21) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 50.17 | 241. | -16. | -1.78 | 46.4 | 44.9 |
| Terrain Sample in Aeolis Dorsa: ESP_079461_1745 ESP_079738_1745 (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 | -5.66 | 154. | -1.8 | -23.0 | 59.6 | 61.6 |
| Aligned Pits in North Polar Layered Deposits: ESP_079474_2645 ESP_079513_2645 (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 | 84.43 | 133. | -8.9 | 5.135 | 60.2 | 59.6 |
| West Olympia Region Polar Aeolian-Ice Landforms: ESP_079779_2600 ESP_079660_2600 (Interval in Earth days: 9) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 79.77 | 91.2 | 0.43 | 15.04 | 57.3 | 56.2 |
| Crater in Arabia Terra: ESP_079664_2185 ESP_079519_2185 (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 | 38.16 | 6.10 | 7.88 | -6.68 | 43.8 | 44.6 |
| Barchan Dunes in North Polar Layered Deposits: ESP_079724_2645 ESP_080053_2645 (Interval in Earth days: 26) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.33 | 137. | 2.16 | 16.70 | 59.9 | 60.7 |
| Fresh Crater Surrounded by Amazonis Planitia Lava Plains with Asymmetry: ESP_079697_2115 ESP_079763_2115 (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 | 31.09 | 186. | 9.02 | -7.51 | 44.3 | 46.0 |
| Possible Vent Region within Volcanic Plains: ESP_079677_1830 ESP_080033_1830 (Interval in Earth days: 28) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.796 | 17.0 | -3.4 | 19.86 | 55.4 | 54.3 |
| Crater-Delineating Mounds in Chryse Planitia: ESP_079784_2055 ESP_079929_2055 (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 | 25.44 | 333. | -7.9 | 10.79 | 47.2 | 46.1 |
| Scalloped Cliff Formations : ESP_079343_2640 ESP_079237_2640 (Interval in Earth days: 8) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.86 | 111. | -8.8 | 5.451 | 59.9 | 59.4 |
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