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.
| Light-Toned Materials Eroding from Ponded Materials in Kontum Crater: ESP_012730_1475 ESP_020866_1475 (Interval in Earth days: 634) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -32.1 | 292. | 5.03 | -17.8 | 46.0 | 54.9 |
| Crater Wall Carving in MOC Image E0300089: ESP_013828_1360 ESP_013683_1360 (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 | -43.4 | 196. | 18.3 | 8.46 | 37.6 | 38.3 |
| Gullies in Southern Hemisphere Crater: ESP_013749_1410 ESP_013894_1410 (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 | -38.8 | 195. | -16. | -5.65 | 38.5 | 37.6 |
| Recent 10 Kilometer Diameter Crater in Ares Vallis: ESP_013335_1975 ESP_020772_1975 (Interval in Earth days: 580) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.40 | 329. | 1.40 | 17.37 | 58.3 | 58.8 |
| Ridge in Coprates Chasma: ESP_013547_1655 ESP_014048_1655 (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 | -14.4 | 305. | 5.36 | 24.80 | 38.4 | 32.4 |
| Layering in Argyre Planitia Sinuous Ridge: ESP_012927_1245 ESP_013626_1245 (Interval in Earth days: 55) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -55.1 | 318. | 1.77 | -23.3 | 48.2 | 46.0 |
| Stratigraphic Relations in THEMIS Image V11134006 in Sinus Meridiani: ESP_013703_1800 ESP_021984_1800 (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 | -0.14 | 2.99 | 25.0 | 10.04 | 41.4 | 46.9 |
| Very Fresh Small Crater in Hesperia Planum: ESP_013976_1670 ESP_020279_1670 (Interval in Earth days: 491) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.8 | 113. | -1.1 | 19.13 | 35.3 | 54.4 |
| Exposure of Polar Layered Deposits Not Well Observed: ESP_013886_0875 ESP_022748_0875 (Interval in Earth days: 691) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.4 | 165. | 4.63 | 10.95 | 71.0 | 71.9 |
| Layered Bedrock on the Floor of an Impact Crater: ESP_012881_1880 ESP_013158_1880 (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 | 8.116 | 125. | 0.85 | -24.8 | 56.6 | 55.9 |
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