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.
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 |
Northern Plains West of Erebus Montes: ESP_016782_2205 ESP_028531_2205 (Interval in Earth days: 915) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 40.06 | 182. | -7.6 | 11.26 | 42.3 | 55.0 |
Aram Chaos Mineralogical Variability: ESP_016605_1830 ESP_086812_1830 (Interval in Earth days: 5470) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 2.889 | 339. | -8.3 | -23.3 | 46.9 | 47.0 |
Terrain South of Newcomb Crater: ESP_016736_1520 ESP_068970_1525 (Interval in Earth days: 4070) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -27.6 | 5.59 | 4.65 | -7.50 | 65.7 | 63.9 |
Potential Rhythmic Layering in East Gale Crater with Hydrated Signature: ESP_016375_1750 ESP_016520_1750 (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 | -5.15 | 138. | 1.01 | 18.09 | 48.0 | 48.2 |
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 |
Dissected Wrinkle Ridge Surrounded by Viscous Flows in Elysium Planitia: ESP_016572_1875 ESP_016150_1875 (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 | 7.515 | 157. | 16.0 | 25.58 | 42.9 | 38.9 |
Ejecta Flow and Obstacle at Arandas Crater: ESP_016776_2225 ESP_016842_2225 (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 | 42.39 | 344. | 4.98 | -9.79 | 41.8 | 43.0 |
Field of Small Volcanoes Northeast of Ascraeus Mons: ESP_016489_1945 ESP_017122_1945 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 14.35 | 263. | 7.23 | -11.9 | 41.0 | 45.5 |
Ridged Material in Viking Image 693A34: ESP_016359_1910 ESP_016992_1910 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 10.86 | 212. | 13.8 | -2.12 | 40.6 | 45.5 |
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