Valentin Burki
Biographic Data
| ID | 6384048 |
|---|---|
| NAME | Valentin Burki |
| GIVEN NAMES | Valentin |
| FAMILY NAME | Burki |
| SIGNATURE | BURKI V |
| AFFILIATIONS | Geological Survey of Norway, N-7491 Trondheim, Norway, Department of Earth Science, University of Bergen, Allegaten 41, N-5007 Bergen, Norway |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 1 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2008 |
| LATEST PUBLICATION YEAR | 2009 |
| H-INDEX | 1 |
Glacial remobilization cycles as revealed by lateral moraine sediment, Bødalsbreen glacier foreland, western Norway
The proglacial area of Bødalsbreen glacier in western Norway contains nine moraine ridges formed at the maximum of the `Little Ice Age' (~AD 1755) and during the subsequent glacier retreat (AD 1767—2000). The frontal moraines are composed of a sandy diamicton, whereas the lateral ones consist of only boulder-sized clasts without any matrix. These lateral moraines seemingly are composed of a very high proportion of mature clasts, a notion supporte…
A photogrammetric digital elevation model of the Bødalen valley saw-tooth moraine complex, western Norway
Please click here to download the map associated with this article. Thorough geomorphological and geophysical investigations rely on high quality digital elevation models (DEM). Many areas in the developed world are covered by DEMs through national ordnance surveys or similar organizations. However, these DEMs are often of quite low resolution and do not allow detailed geomorphological investigations. One way to overcome this problem is to photog…
Glacial remobilization cycles as revealed by lateral moraine sediment, Bødalsbreen glacier foreland, western Norway
The proglacial area of Bødalsbreen glacier in western Norway contains nine moraine ridges formed at the maximum of the `Little Ice Age' (~AD 1755) and during the subsequent glacier retreat (AD 1767—2000). The frontal moraines are composed of a sandy diamicton, whereas the lateral ones consist of only boulder-sized clasts without any matrix. These lateral moraines seemingly are composed of a very high proportion of mature clasts, a notion supporte…
A photogrammetric digital elevation model of the Bødalen valley saw-tooth moraine complex, western Norway
Please click here to download the map associated with this article. Thorough geomorphological and geophysical investigations rely on high quality digital elevation models (DEM). Many areas in the developed world are covered by DEMs through national ordnance surveys or similar organizations. However, these DEMs are often of quite low resolution and do not allow detailed geomorphological investigations. One way to overcome this problem is to photog…
Glacial remobilization cycles as revealed by lateral moraine sediment, Bødalsbreen glacier foreland, western Norway
The proglacial area of Bødalsbreen glacier in western Norway contains nine moraine ridges formed at the maximum of the `Little Ice Age' (~AD 1755) and during the subsequent glacier retreat (AD 1767—2000). The frontal moraines are composed of a sandy diamicton, whereas the lateral ones consist of only boulder-sized clasts without any matrix. These lateral moraines seemingly are composed of a very high proportion of mature clasts, a notion supporte…
Cryospheric studies and observations (2 works) · Foreland basin (2 works) · Geology (2 works) · Geomorphology (2 works) · Glacier (2 works) · Landslides and related hazards (2 works) · Moraine (2 works) · Bespoke (1 work) · Cartography (1 work) · Clastic rock (1 work)