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.
| Geologic Contact Between Landslides and Blocky Deposit on Floor of Melas Ch: ESP_016739_1715 ESP_018941_1715 (Interval in Earth days: 172) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.58 | 282. | -8.3 | 8.612 | 54.0 | 57.9 |
| Candidate MSL Landing Site Near Putative Chloride: ESP_016710_1745 ESP_016855_1745 (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 | -5.66 | 353. | -8.3 | 10.34 | 52.1 | 52.0 |
| Crossing Wrinkle Ridges and Secondaries in Hesperia Planum: ESP_016310_1545 ESP_016666_1545 (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 | -25.2 | 115. | 3.44 | 15.21 | 59.1 | 62.7 |
| Well-Exposed Layered Deposits in Nilosyrtis Mensae Region: ESP_016430_2095 ESP_019120_2095 (Interval in Earth days: 210) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 29.05 | 72.6 | 0 | -14.9 | 40.2 | 49.6 |
| Southern Margin of Mantle Material within Crater: ESP_016542_1435 ESP_025403_1435 (Interval in Earth days: 690) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -36.1 | 262. | 6.93 | 27.81 | 69.4 | 67.9 |
| Crater with Sharp Rim and Elongated Secondaries: ESP_016810_2260 ESP_017232_2260 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 45.63 | 135. | 1.70 | -9.75 | 42.9 | 43.1 |
| Well-Preserved 10-Kilometer Diameter Impact Crater: ESP_016745_1810 ESP_017523_1810 (Interval in Earth days: 60) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 0.765 | 116. | 0 | -11.5 | 48.4 | 53.4 |
| Eastern Portion of Very Well-Preserved 11-Kilometer Diameter Impact Crater: ESP_016701_2210 ESP_017123_2210 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 40.51 | 231. | 7.50 | -3.19 | 41.3 | 41.6 |
| Central Uplift and Layered Materials on Crater Floor: ESP_016435_2200 ESP_017714_2200 (Interval in Earth days: 99) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 39.61 | 294. | 0 | 10.58 | 42.2 | 40.7 |
| Scalloped Features in Deuteronilus Mensae: ESP_016313_2265 ESP_016590_2265 (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 | 46.17 | 23.3 | 8.14 | -8.96 | 44.5 | 44.6 |
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