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.
| 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 |
| Landforms above Subsurface Radar Observations of South Polar Cap: ESP_092633_0995 ESP_084840_0995 (Interval in Earth days: 607) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -80.2 | 200. | -21. | -7.26 | 61.7 | 69.1 |
| 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 |
| 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 |
| Thermal Anomaly in Young Lava Flows of Elysium Mons: ESP_092633_1960 ESP_092989_1960 (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 | 15.59 | 165. | 13.9 | 2.663 | 57.1 | 53.8 |
| 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 |
| Possible Chloride-Rich Deposit Southwest of Amenthes Planum: ESP_092240_1810 ESP_092464_1810 (Interval in Earth days: 18) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 0.947 | 101. | -2.4 | 22.95 | 53.1 | 49.2 |
| Channels in Southern Mid-Latitudes: ESP_092160_1445 ESP_092094_1445 (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 | -34.9 | 132. | -25. | -11.2 | 47.5 | 47.1 |
| Interesting Domes and Channels Cutting Ridges: ESP_092003_1380 ESP_092583_1380 (Interval in Earth days: 45) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -41.7 | 97.7 | -13. | 15.44 | 49.5 | 40.1 |
| Bedform Change Detection near Mawrth Vallis: ESP_092152_2045 ESP_092297_2045 (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 | 24.30 | 340. | -1.8 | 12.24 | 67.1 | 65.7 |
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