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.
| Incised Gullies: ESP_085346_1395 ESP_085491_1395 (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 | -39.9 | 46.0 | 6.28 | 26.83 | 46.8 | 47.7 |
| Eroded Layered Bedrock: ESP_085567_1555 ESP_085923_1555 (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 | -24.3 | 132. | -6.1 | 16.95 | 42.3 | 45.7 |
| Dune Monitoring in North Mid-Latitude Bonestell Crater: ESP_085388_2220 ESP_085520_2220 (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 | 41.8 | 329. | -0.3 | -22.8 | 57.2 | 57.0 |
| Alluvial Fans in Kasei Valles: ESP_085574_2030 ESP_085640_2030 (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 | 22.67 | 293. | 15.8 | 1.691 | 42.0 | 42.6 |
| Large Isolated Landform at Chryse Planitia Margin: ESP_085402_1945 ESP_085547_1945 (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 | 14.22 | 310. | 5.37 | 29.46 | 39.9 | 37.2 |
| Inverted Channel in Noachis Terra: ESP_085453_1585 ESP_085519_1585 (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 | -21.1 | 2.69 | 9.81 | -7.34 | 38.4 | 40.4 |
| Triangular Faceted Spurs in East Candor Chasma: ESP_085693_1740 ESP_085838_1740 (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 | -6.03 | 291. | -3.9 | 20.84 | 37.7 | 36.9 |
| Ridges near Vernal Crater: ESP_085651_1840 ESP_086218_1840 (Interval in Earth days: 44) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 3.944 | 356. | 3.12 | -8.10 | 36.7 | 40.5 |
| Margin of Athabasca Valles Lava: ESP_085672_1835 ESP_085738_1835 (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 | 3.686 | 142. | 7.88 | -7.30 | 36.3 | 37.7 |
| Layered Deposits in Melas Chasma: ESP_085535_1695 ESP_085746_1695 (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 | -10.1 | 284. | -7.5 | 8.858 | 37.4 | 38.0 |
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