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.
| Collapsed Terrain in Osuga Valles Depression and Part of Relict Channel: ESP_067678_1650 ESP_068008_1650 (Interval in Earth days: 26) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -14.8 | 322. | 4.26 | -24.2 | 39.6 | 45.2 |
| Crater Fill Materials: ESP_067663_1360 ESP_076631_1360 (Interval in Earth days: 699) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -43.7 | 15.7 | 4.85 | -5.40 | 50.8 | 51.6 |
| Searching for Slope Features: ESP_067410_1515 ESP_076853_1515 (Interval in Earth days: 735) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -28.1 | 76.1 | 5.88 | -23.1 | 40.2 | 47.0 |
| Gullies Mantling and Glaciers near Dao Vallis: ESP_067581_1440 ESP_067713_1440 (Interval in Earth days: 10) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.6 | 91.8 | 4.62 | -9.42 | 45.3 | 48.1 |
| Outcrops of Fluvial Deposits in Mesa Flank: ESP_067605_1760 ESP_066510_1760 (Interval in Earth days: 86) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -3.80 | 152. | 5.52 | -6.48 | 38.9 | 45.6 |
| Layering in Arabia Terra: ESP_067505_1845 ESP_067637_1845 (Interval in Earth days: 10) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 4.307 | -0.0 | 8.59 | -8.44 | 40.6 | 41.6 |
| A Technicolor Mound near Oxia Planum: ESP_066622_2000 ESP_074430_2000 (Interval in Earth days: 608) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 19.88 | 332. | 5.69 | 22.84 | 57.4 | 63.3 |
| Crater near Dao Vallis: ESP_067040_1440 ESP_066209_1440 (Interval in Earth days: 65) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.8 | 93.1 | 3.28 | -19.1 | 40.0 | 43.0 |
| Valleys in Crater Northeast of Argyre Region: ESP_067229_1500 ESP_067361_1500 (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 | -29.7 | 334. | 7.83 | -10.6 | 39.0 | 41.4 |
| South Polar Layered Deposits: ESP_067270_0910 ESP_067124_0910 (Interval in Earth days: 12) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -89.0 | -2.7 | 24.9 | 27.39 | 75.7 | 73.1 |
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