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- W2201473401 abstract "AbstractDepositional terraces of diverse origin are common in Norwegian fjord valleys. They differ subtly morphologically and may be difficult to distinguish from one another without detailed field and stratigraphic investigation. We used LiDAR elevational data to describe previously identified glaciofluvial, glaciodeltaic, fluvial, and fluviodeltaic terraces in the Malselv valley, northern Norway, and show how they differ morphologically. Fluvial terraces are divided into two subtypes based on their difference in morphology. One type shows an undulating surface, often with a ridge-and-swale topography (scroll bars) associated with lateral accretion of moderate-to-high-sinuosity (meandering) channels, while the other shows remains of channels and braid bars associated with low-sinuosity channels. Fluviodeltaic terraces are generally flat and featureless, probably as a result of wave and tidal reworking of the terrace surface as it was raised above sea level. Glaciofluvial terraces show braided channel for..." @default.
- W2201473401 created "2016-06-24" @default.
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- W2201473401 date "2015-10-02" @default.
- W2201473401 modified "2023-09-25" @default.
- W2201473401 title "Using LiDAR data to characterize and distinguish among different types of raised terraces in a fjord-valley setting" @default.
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- W2201473401 doi "https://doi.org/10.1080/11035897.2015.1111409" @default.
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