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.
| Hillslope Morphologies near Murray Crater: ESP_093627_1555 ESP_092981_1555 (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 | -24.1 | 28.3 | 25.6 | 5.313 | 32.6 | 36.0 |
| Irregular Cellular Structures around Crater in Southern Mid-Latitudes: ESP_093680_1285 ESP_093614_1285 (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 | -50.9 | 28.5 | -9.1 | 10.29 | 47.8 | 45.9 |
| Gullies in Crater in Terra Cimmeria: ESP_093779_1420 ESP_093344_1420 (Interval in Earth days: 34) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.4 | 201. | 5.23 | -10.2 | 40.2 | 38.1 |
| Portion of Mound in Gale Crater: ESP_093623_1750 ESP_093333_1750 (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 | -5.00 | 137. | -2.7 | -16.8 | 36.1 | 39.3 |
| Fan Deposit: ESP_093521_1335 ESP_093442_1335 (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 | -46.1 | 48.4 | 1.80 | -19.7 | 42.5 | 43.4 |
| Potential Compound Dune in USGS Dune Database Entry Number 1781-552: ESP_093569_1245 ESP_093147_1245 (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 | -55.2 | 178. | 9.74 | 23.62 | 48.1 | 43.6 |
| Dunes with Erosionally-Resistant Layers in Ross Crater: ESP_093751_1220 ESP_093329_1220 (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 | -57.5 | 251. | -11. | 12.7 | 53.4 | 47.2 |
| Potential Compound Dune in USGS Dune Database Entry Number 1787-4570: ESP_093648_1225 ESP_092857_1225 (Interval in Earth days: 62) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -57.0 | 178. | 25.2 | 7.918 | 49.4 | 45.1 |
| Chasma Australe Layering: ESP_093559_0940 ESP_093586_0940 (Interval in Earth days: 2) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.8 | 95.8 | 28.9 | 15.35 | 70.0 | 71.4 |
| Diverse Minerology in Nili Fossae: ESP_093625_2040 ESP_085371_2040 (Interval in Earth days: 643) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 23.50 | 76.7 | 25.0 | -7.95 | 49.8 | 45.8 |
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