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.
| Sinuous Ridges on Both Sides of Scarp in Aeolis Planum: ESP_084920_1730 ESP_085065_1730 (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 | -6.73 | 151. | -1.5 | 13.33 | 35.5 | 34.1 |
| Landforms above Subsurface Radar Observations of South Polar Cap: ESP_085104_0975 ESP_085012_0975 (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 | -82.1 | 188. | 7.05 | -7.33 | 73.9 | 73.3 |
| Possible Light-Toned Deposits in Eastern Iani Chaos: ESP_085203_1780 ESP_093378_1780 (Interval in Earth days: 637) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -1.97 | 345. | -0.8 | 26.05 | 35.9 | 37.1 |
| Sinuous Flows in Mamers Valles: ESP_085149_2230 ESP_085294_2230 (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 | 42.88 | 14.2 | -7.1 | 7.44 | 61.7 | 58.8 |
| Fan and Ridges in Southern Gale Crater: ESP_085171_1745 ESP_077088_1745 (Interval in Earth days: 629) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.59 | 137. | 14.5 | -1.72 | 34.1 | 39.5 |
| Lighter-Toned Deposits in Young Crater: ESP_085271_1870 ESP_085337_1870 (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 | 7.156 | 287. | -1.6 | -20.0 | 38.2 | 39.4 |
| Channel Northeast of Hellas Planitia: ESP_084975_1630 ESP_092794_1630 (Interval in Earth days: 609) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -16.7 | 91.4 | 0 | 27.65 | 34.7 | 37.4 |
| Mesa Stratigraphy at Terby Crater: ESP_085068_1525 ESP_085213_1525 (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 | -27.1 | 74.1 | -4.4 | 13.86 | 37.8 | 37.8 |
| Small Pedestal Crater: ESP_085103_2135 ESP_085169_2135 (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 | 33.31 | 189. | 9.68 | -7.03 | 54.3 | 54.3 |
| Glacial Ridges in Arsia Mons Fan-Shaped Deposit: ESP_085207_1745 ESP_085352_1745 (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 | -5.44 | 236. | 2.19 | 25.29 | 35.1 | 33.5 |
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