Carpathians ; Dating ; High mountain ; Little ice age ; Mountain ; Mudflow ; Poland ; Slope ; Slope dynamics ; Tatra Mountains
during the Little Ice Age. At present, debris flow activity is limited to apex sector of talus slopes. Only sporadically debris flows affect a whole slope. - (DG)
Dating ; Debris flows ; Holocene ; Lichenometry ; Little ice age ; Paleogeography ; Poland ; Quaternary ; Tatra Mountains
of the investigated debris flows were triggered during the later part of the Little Ice Age, due to alluviation. During the last hundred years, only a few debris flows have occurred.
In this river system whose water is derived mainly from snowmelt, an analysis of nine years of hydrologic data shows little variation in runoff, but great variation in sediment yield, mostly as a result of soil erosion caused by human agency. - (DWG)
In this paper the Holocene glacial record, as inferred from the radiocarbon-dated section with alternating minerogenic and organic sediments beyond the maximum Little Ice Age marginal position of Blaisen, is described and discussed in relation
Relatively little attention has been paid to the Holocene evolution of the rivers since the end of the last glaciation, although the main trends were thought to be understood. Nevertheless, a considerable number of studies have been carried out
British Columbia ; C14 dating ; Canada ; Glacial features ; Glacier surges ; Lake level ; Little ice age ; Moraines ; Paleo-environment ; Proglacial lake
This paper presents results of a palynological analysis of a 15.5 m sediment core from Lake Naivasha. The core spans a little more than the last 20,000 years. The record is long enough to include the last glacial maximum in temperate latitudes
Although there is a debate about the alleged significance of changes in farm occupancy to the management of the farmed landscape, there is little empirical research detailing the relationships. With use of a longitudinal analysis of over 250 farm
The structure of four Vistulian terraces and two Holocene Levels of the flood plain is presented. A dating of organic deposits showed that a cut off of meanders and covering of peats by muds took place about 3 100 BP, 1 000 BP and in Little Ice Age
and adds little to the total volume during spring. Moreover, during the snowmelt, sediments are finer than those produced by rainstorms due to the hydrologic conditions and the different sediment sources.
This monograph is concerned with spatial changes caused by legal regulations, a topic which has hitherto received little attention in the geographical literature. Part A collates the most important legal regulations on rural settlement. In part B
New sites in the Vistula valley between Cracow and Niepołomice were discussed and 7 generations of Holocene meanders was distinguished, which cut off in 8 000, 6 700-6 200, 5 400-5 200, 4 400-4 000, 3 000, 2 200-2 100 BP and Little Ice Age. A clear
Arctic Region ; Cold area ; Glacier ; Glacier fluctuation ; Glacier mass balance ; Holocene ; Little ice age ; Precipitation ; Quaternary ; Research technique ; Spitsbergen ; Svalbard ; Temperature