| DOM_2020-0032 | |
|---|---|
| Model information | |
| data doi | 10.5281/zenodo.6320818 |
| easting | 527222.94 |
| island | Spitsbergen |
| land | Torell Land |
| locality | Burgerbukta |
| northing | 8552998.38 |
| crs epsg | 32633 |
| Technical specs | |
| acq. camera lens | 10.26 |
| acq. camera model | Hasselblad L1D-20c |
| acq. date | 2020-08-26 |
| acq. georeferencing | built-in GPS |
| proc. alignment accuracy | Highest |
| proc. camera stations | 170 |
| proc. camera total error | 1.9409 m |
| proc. coverage area | 2.27 km2 |
| proc. dc filter conf min | 5 |
| proc. dem point density | 8.49 points/m2 |
| proc. dem resolution | 0.0343 m/pix |
| proc. depth map accuracy | High |
| proc. flying altitude | 597 m |
| proc. ground resolution | 0.0172 m/pix |
| proc. mesh filter con comp | 99 |
| proc. sc filter proj acc | 0.3 |
| proc. sc filter recon uncert | 70 |
| proc. sc filter reproj error | 5 |
| proc. software | Agisoft Metashape |
| proc. software version | 1.7.1.11797 |
Digital outcrop model of the Kruseryggen and Urnetoppen cliffsides in Burgerbukta, Southern Spitsbergen. The profile shows an outcrop of the Mid Carboniferous to Late Permian deposits. The succession shows (mid-) late Carboniferous alluvial red-bed deposits of the Hyrnefjellet Formation (Fm.) which grade upwards into being interbedded by shallow-marine sandy deposits. Overlying the Hyrnefjellet is the Parallic to shallow marine sandstone and carbonates of the late Carboniferous to early Permian Treskelodden Fm. which is completely carbonate dominated towards its top. Overlying the Treskelodden Fm. is inner shelf chert deposits of the late Permian Kapp Starostin Fm. The boundary between the Treskelodden and Kapp Starostin Fm’s in Burgerbukta records a major unconformity. Both the Hyrnefjellet and Treskelodden Fm’s were affected by syn-sedimentary faulting in Burgerbukta area evidenced by the large amount of conglomerate deposits adn small growth faults. In addition, most clear in the Treskelodden and Kapp Starostin Fm’s is Tertiary reverse faults formed during the West Spitsbergen Fold and Thrust belt.