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 in Walls of Well-Preserved Impact Crater in Tartarus Montes: ESP_019222_2055 ESP_019367_2055 (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 | 25.03 | 167. | -7.6 | 5.969 | 49.8 | 49.8 |
| Exposure of North Polar Layered Deposits: ESP_019343_2685 ESP_028008_2685 (Interval in Earth days: 675) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 88.28 | 50.8 | -14. | -24.3 | 74.8 | 73.1 |
| Flow Material in Equatorial Crater: ESP_019267_1720 ESP_024858_1720 (Interval in Earth days: 436) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.05 | 23.2 | -8.4 | -26.9 | 58.1 | 46.5 |
| Alpine Glacier: ESP_019213_2210 ESP_019503_2210 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 40.86 | 51.3 | -8.0 | 14.46 | 51.2 | 52.7 |
| Steep North Polar Boundary Scarp: ESP_018943_2655 ESP_019181_2655 (Interval in Earth days: 19) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 85.36 | 186. | 0 | -13.2 | 67.0 | 70.6 |
| Thermally-Distinct Material at Distal Coogoon Valles: ESP_019084_1980 ESP_060437_1980 (Interval in Earth days: 3222) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.85 | 336. | -5.5 | 5.547 | 49.5 | 37.7 |
| Well-Preserved Impact Crater in Arabia Terra: ESP_019162_1975 ESP_019439_1975 (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 | 17.23 | 5.48 | 7.48 | -19.6 | 48.9 | 52.7 |
| Cluster of Zunil Crater Secondaries: ESP_019064_1835 ESP_019209_1835 (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 | 3.656 | 163. | 2.92 | 17.53 | 52.6 | 51.6 |
| Layered Terrains in Aeolis Planum: ESP_018972_1755 ESP_019605_1755 (Interval in Earth days: 50) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.27 | 154. | 15.7 | -5.86 | 55.1 | 56.0 |
| Steep North-Polar Boundary Scarp: ESP_018957_2655 ESP_019195_2655 (Interval in Earth days: 19) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 85.25 | 160. | 3.29 | -9.91 | 67.0 | 70.5 |
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