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.
| Region Dubbed Troy: ESP_082004_0950 ESP_082005_0950 (Interval in Earth days: 0) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.0 | 258. | -8.4 | -25.8 | 88.0 | 90.1 |
| Fan in Lohse Crater: ESP_081828_1355 ESP_081762_1355 (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 | -44.2 | 342. | -14. | 1.08 | 71.0 | 70.8 |
| Olympus Mons: ESP_081700_1980 ESP_081634_1980 (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 | 17.84 | 227. | 4.55 | 24.18 | 57.6 | 55.6 |
| The Oldest Sedimentary Rocks on Mars: ESP_049832_1560 ESP_049898_1560 (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 | -23.9 | 57.3 | -1.5 | -19.2 | 32.8 | 34.7 |
| Streamlined Landforms adjacent to Shalbatana Vallis: ESP_081512_1890 ESP_080800_1890 (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 | 8.966 | 318. | 28.8 | 14.43 | 54.2 | 53.2 |
| Secondary Crater Field in Oxia Planum: ESP_081485_1985 ESP_073098_1985 (Interval in Earth days: 653) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 18.46 | 336. | 7.11 | 23.55 | 55.9 | 56.9 |
| Possible Salt Diapir: ESP_081566_1730 ESP_082054_1730 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.90 | 288. | 3.74 | -10.0 | 59.0 | 59.2 |
| Dune Monitoring in Northern Mid-Latitude Crater: ESP_081456_2340 ESP_089763_2340 (Interval in Earth days: 647) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 53.71 | 41.5 | 8.54 | -0.90 | 62.9 | 55.6 |
| Small Gullies on Ridge and Lobate Flows on Crater Floor: ESP_081539_1360 ESP_081882_1360 (Interval in Earth days: 27) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -43.7 | 309. | 13.8 | -16.5 | 72.5 | 70.3 |
| Aeolis Dorsa Branching Fluvial Deposits: ESP_081439_1735 ESP_081584_1735 (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 | -6.30 | 154. | 9.46 | 27.06 | 58.5 | 56.8 |
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