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.
| Bedrock Exposure in Landslide Scarp: ESP_020879_1670 ESP_021657_1670 (Interval in Earth days: 61) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.9 | 293. | 5.19 | -7.68 | 52.2 | 46.1 |
| Faulted Crater in Claritas Rupes: ESP_020564_1455 ESP_020841_1455 (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 | -34.2 | 256. | 4.03 | -21.5 | 57.7 | 56.0 |
| Eroded Pitted Materials on Floor 90-Kilometer Diameter Impact Crater: ESP_020553_1650 ESP_020698_1650 (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 | -14.6 | 193. | 5.79 | 20.85 | 54.1 | 52.0 |
| Outcrop of Rhythmic Stratigraphy Southeast of Crommelin Crater: ESP_020534_1825 ESP_021523_1825 (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 | 2.225 | 350. | 5.74 | -9.90 | 54.9 | 53.6 |
| Dunes on Crater Floor: ESP_020709_1350 ESP_020854_1350 (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 | -44.4 | 259. | -4.8 | 8.47 | 59.5 | 56.3 |
| Streamlined Form Surrounded by Pitted Materials in Hale Crater: ESP_020667_1440 ESP_030069_1440 (Interval in Earth days: 733) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.5 | 324. | -1.4 | -14.8 | 57.0 | 49.7 |
| Heavily Pitted Streamlined Ejecta Lobe Originating from Mojave Crater: ESP_020548_1875 ESP_028539_1875 (Interval in Earth days: 623) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 7.169 | 328. | -7.9 | 11.85 | 56.9 | 51.8 |
| Tongue-Shaped Flow Feature on Mound East of Hellas Region: ESP_020741_1445 ESP_020886_1445 (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 | -35.0 | 105. | -8.1 | 7.29 | 56.5 | 53.3 |
| Well-Preserved 3-Kilometer Diameter Impact Crater in Terra Sirenum: ESP_020725_1525 ESP_029283_1525 (Interval in Earth days: 667) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -27.3 | 179. | 6.77 | 24.62 | 53.9 | 54.9 |
| Possible Olivine in East Thaumasia Planum: ESP_020905_1525 ESP_083306_1525 (Interval in Earth days: 4862) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -27.0 | 305. | 4.56 | 13.84 | 52.0 | 45.6 |
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