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.
| Floor of Peraea Cavus: ESP_021717_1500 ESP_021572_1500 (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 | -29.8 | 95.3 | 17.1 | 6.52 | 40.6 | 43.4 |
| Candidate New Gully Flow Formed between 15 May 2009 and 3 March 2011: ESP_021914_1475 ESP_022336_1475 (Interval in Earth days: 32) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -32.3 | 118. | 3.26 | -10.0 | 39.2 | 35.9 |
| Impact Crater into Heavily Mantled Pole-Facing Slope: ESP_021771_1505 ESP_021626_1505 (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 | -29.2 | 63.2 | -8.3 | -19.5 | 41.9 | 44.7 |
| Fractures and Uplifted Portion of Floor of Echus Chasma: ESP_021908_1810 ESP_021842_1810 (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 | 0.856 | 279. | -17. | 4.9 | 50.1 | 49.2 |
| Recent 5-Kilometer Diameter Crater with Gullies and Bedrock Exposures: ESP_021695_1480 ESP_022684_1480 (Interval in Earth days: 78) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -31.4 | 337. | 7.22 | -2.08 | 41.7 | 33.5 |
| Northern Part of Asimov Crater Ring Trough: ESP_021694_1330 ESP_021760_1330 (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 | -46.4 | 4.90 | 21.1 | 4.178 | 42.9 | 43.4 |
| Crater with Channel-Like Feature: ESP_021907_1710 ESP_022329_1710 (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 | -8.79 | 307. | -6.2 | -20.3 | 44.7 | 40.7 |
| Central Uplift with Layers and Clays: ESP_021688_1325 ESP_021754_1325 (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 | -47.2 | 170. | 2.61 | -14.9 | 44.6 | 45.1 |
| Crater and Landslides: ESP_021704_1625 ESP_022205_1625 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -17.3 | 90 | 2.26 | 26.21 | 43.6 | 35.7 |
| Lava Flow Features in Marte Vallis: ESP_021964_2015 ESP_030232_2015 (Interval in Earth days: 645) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 21.01 | 186. | 4.43 | -13.0 | 60.8 | 64.2 |
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