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These fracture systems have been important for guiding erosion. The maximum depth m of the Sognefjord is at Vadheim, further out. The fjord bottom then rises to the Solund areaand the sea bottom extends westwards at depths of m. The mountains along the Sognefjord rise gradually eastward from about m in the coastal region to altitudes above metres in Jotunheimen Fig.
The highest mountain adjacent to the Sognefjord is Bleia mand the largest relief along the fjord of m is found here. However, the average relief along the fjord is about metres. Quaternary glacial erosion in the Sognefjord drainage basin Fig. In many places the paleic surface is preserved more or less unaltered and the paleic surface and the present landscape commonly occur together Fig.
The consistent and gradually rising summit level eastwards along the Sognefjord Fig. However, the preglacial valley floor is difficult to reconstruct accurately along the present fjord Fig. Assuming that consistent summit levels and the wide, high-lying valley represent the paleic, pre-Quaternary land surface, the present relief represents the total Quaternary erosion and denudation.
Both glacial and fluvial erosion are selective and follows zones of bedrock weakness, but at different rates.
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Therefore, the relative amounts of glacial and fluvial erosion must have varied greatly from site to site. The total Quaternary erosion and denudation is quantified by subtracting the present landscape from the reconstructed paleic surface.
Excluding the Quaternary sediments at the bottom of the Sognefjord, the volume difference between the reconstructed paleic surface and present topography is km3. Video from the Sognefjord and the surrounding nature Erosion Rates The volume of km3 of eroded bedrock distributed over the Sognefjord drainage basin 12, km2yields an average vertical erosion of m.
Supposing that the erosion of the Sognefjord basin started at the beginning of the first significant Quaternary glaciations in Scandinavia 2. The volumes of large submarine fans on the mid-Norwegian continental shelf deposited during the last 2. Some of the increased sedimentation may be the result of fluvial erosion following the uplift, but it is difficult to separate from glacial erosion.
During the Quaternary there have been several glacials and interglacials. The first significant expansion of the Scandinavian ice sheet occurred at 2. Minor glacier expansions, however, are recorded at 5. The period between 2. This is of similar magnitude as erosion rates calculated for modern Norwegian glaciers, which range from 1. Using the average relief along the fjord basin mthe mean erosion rate over the last 2.
The highest rate of glacial erosion may be estimated from the maximum relief along the Sognefjord m. From this, the maximum average erosion rate over the last 2. Taking into account the selective nature of ice streams, annual erosionrates for ice streams in the Sognefjord drainage basin probably varied between 1. These variables critically affect the effectiveness of abrasion and other erosional processes. July trade surplus narrowed to KRW Hong Kong's Hang Seng climbed 0. On the downside, Geely Automobile lost 1.
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What is a fjord | NORWEGIAN FJORDS - Western Norway
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What is a fjord
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Female, 40 years old, L4, two joints treated. Patient had injection local only at the facet joint. At the end of the procedure the patient moved herself from the table and walked under her own power out of the procedure room and was discharged shortly after with no pain prescription provided other than over the counter pain relief medicines.
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Male, 42 year old, L5, two joints treated. Patient had an injected local only at the facet joint.HOME
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