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.
Well-Preserved 5-Kilometer Diameter Impact Crater in Acidalia Planitia: ESP_016131_2140 ESP_017054_2140 (Interval in Earth days: 72) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 33.45 | 315. | -6.9 | 5.242 | 41.9 | 40.4 |
Steep Crater Slope: ESP_015993_1450 ESP_016494_1450 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -34.5 | 131. | 0.90 | 23.82 | 61.2 | 66.6 |
Bright Layers in Columbus Crater: ESP_016083_1505 ESP_016584_1505 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -29.1 | 193. | -4.3 | 21.15 | 59.1 | 63.9 |
Gullied Slope of 20-Kilometer Diameter Impact Crater in Acidalia Planitia: ESP_016170_2230 ESP_016460_2230 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 42.64 | 329. | 0.01 | 21.35 | 44.4 | 41.3 |
Layered Bedrock in Central Uplift of a Large Crater: ESP_016132_1595 ESP_016765_1595 (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 | -20.3 | 293. | 8.27 | -7.22 | 53.3 | 61.6 |
Athabasca Valles: ESP_016071_1890 ESP_024708_1890 (Interval in Earth days: 673) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 8.934 | 155. | 7.83 | -16.8 | 39.6 | 38.8 |
Deep Bedrock Exposure in Melas Chasma: ESP_016264_1705 ESP_016897_1705 (Interval in Earth days: 50) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.22 | 288. | 7.41 | -7.19 | 48.5 | 55.6 |
Potential MSL Landing Site in Eberswalde Crater: ESP_016065_1560 ESP_016210_1560 (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 | -23.9 | 326. | -28. | -15.6 | 57.2 | 58.1 |
Kunowsky Crater Central Peak with Strong Olivine Signature: ESP_016235_2370 ESP_016314_2370 (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 | 56.79 | 350. | 8.37 | 25.32 | 50.4 | 48.5 |
Possible Fresh Small Crater in Arcadia Planitia: ESP_015898_2225 ESP_041348_2225 (Interval in Earth days: 1983) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 41.98 | 194. | 6.9 | -4.52 | 45.2 | 56.1 |
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