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.
Mesa Island in East Acidalia Planitia: ESP_016301_2250 ESP_016578_2250 (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 | 44.70 | 352. | -3.9 | -20.7 | 44.9 | 45.2 |
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 |
Valleys within Electris Region Deposit: ESP_016664_1420 ESP_045305_1420 (Interval in Earth days: 2232) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.9 | 172. | 1.33 | 28.48 | 72.5 | 72.2 |
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 Impact Crater: ESP_016574_2060 ESP_020042_2060 (Interval in Earth days: 271) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 25.93 | 101. | 6.48 | -8.46 | 39.8 | 57.5 |
Discontinuous Small Channel South of Dao Vallis: ESP_016311_1420 ESP_016588_1420 (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 | -37.6 | 89.5 | 5.56 | -17.0 | 67.7 | 72.4 |
Well-Preserved Impact Crater on Somewhat Older Crater: ESP_016345_2210 ESP_017624_2210 (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 | 40.46 | 231. | -0.3 | 11.17 | 42.8 | 40.6 |
Pristine Channels in Fractured Materials on Crater Floor: ESP_016538_2190 ESP_017171_2190 (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 | 38.77 | 2.06 | 7.68 | -7.08 | 41.1 | 41.9 |
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 |
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