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.
| Troughs overlying South Polar Layered Deposit: ESP_092416_0905 ESP_083622_0905 (Interval in Earth days: 685) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -89.3 | 8.90 | 28.4 | 26.90 | 64.8 | 64.9 |
| Hillslope Morphologies near Eberswalde Crater: ESP_092601_1550 ESP_092812_1550 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -24.7 | 325. | -4.5 | -25.4 | 40.5 | 39.9 |
| Crater-Related Pitted Materials in 3-Kilometer Crater in Nepenthes Planitia: ESP_092411_1960 ESP_092622_1960 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 15.73 | 108. | 5.50 | -22.3 | 59.7 | 59.6 |
| South Polar Glacier Crevasses: ESP_092682_0915 ESP_092589_0915 (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 | -88.6 | 323. | 22.6 | 26.11 | 64.9 | 64.3 |
| Banded or Layered Megabreccia Clasts in Nili Fossae: ESP_092544_1995 ESP_092610_1995 (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 | 19.17 | 76.5 | -1.1 | -26.7 | 61.3 | 62.3 |
| Light Tone Exposures on Floor of Coprates Chasma: ESP_092628_1645 ESP_092259_1645 (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 | -15.1 | 305. | 12.1 | -12.6 | 41.1 | 47.4 |
| Dune Field: ESP_092506_1945 ESP_093007_1945 (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 | 14.45 | 34.8 | 0.29 | -9.08 | 58.4 | 53.5 |
| Crater with Ice Deposit Plus Rim Erosion and Gullies: ESP_092582_1425 ESP_092938_1425 (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 | -36.9 | 126. | -2.7 | -15.6 | 40.6 | 38.8 |
| Rock Glacier-Like Features: ESP_092481_1390 ESP_092257_1390 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -40.4 | 3.96 | 7.89 | -11.8 | 41.4 | 45.6 |
| Hale Crater Gullies Seen in MOC Image R0700653: ESP_092232_1450 ESP_092311_1450 (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 | -34.7 | 324. | 0.47 | 25.97 | 44.4 | 41.2 |
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