The latter is deformed and likely influenced by Pleistocene glacial and/or glaciofluvial
Moreover, the western border both of the reference area and the culture was rather distinctly marked by the not overpassed natural barrier of the Labanoras Woods, covering the area of infertile glaciofluvial
These sites are located in similar lowland settings, overlooking wetland deltas along the glaciofluvial
floodplain of the Tanana River.
Midwestern streams often flow through fluvial and glaciofluvial
deposits that are easily erodible, and tailwaters frequently scour substrates in an attempt to obtain a water flux - sediment load equilibrium (Kondolf 1997).
Sandy soils originate from glaciofluvial
and glaciolacustrine deposits that are wide-spread in north-eastern Germany.
Settings that produce less Ideal sands that may be processed for use as proppant include younger aeolian, glaciodeltaic, and glaciofluvial
environments (Hickin and others, 2010), Examples of unconsolidated frac sand from glaciofluvial
deltaic and aeolian settings are known from northeastern British Columbia, Canada (Hickin and others, 2010).
The presence of perennial streams discharging out of gorges and ravines and transiting a combination of fault zones, adjacent steeply dipping, fractured sedimentary basin rocks, glaciofluvial
outwash, and active karst (Fig.
Controlled burning can support the conservation of many sites of priority habitat type 9010 (*Western Taiga) and, to some extent, habitat 9060 (Coniferous forests on, or connected to, glaciofluvial
eskers) Up until 150 years ago, 1% of the wooded area burned annually.
The north and north-west of the district has moraine and glaciofluvial
sediments of the middle Pleistocene age.
The geological substrate of BPF is formed mainly by moraine upland, made of glaciofluvial
sands, gravels and silts and divided by marshy river valleys.
His main research trend is the Lithuanian Pleistocene glaciolacustrine, glaciofluvial
sediments: their structure and composition, geological heritage and application of distant methods for the research of exogenous Quaternary sediment processes, archaeological camps and settlements.
Soil1 was located at the upper part of a hill on moraine sediments and Soil2 in the depression of the relief on glaciofluvial