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Nysa Depression, central Sudetes Mts, southwestern Poland

part of the Upper Nysa Depression, central Sudetes Mts, southwestern Polanddominated braided rivers of Donjek and Scott type, and locally on alluvial

of Polands Past ; Its a Story That No One Wanted to Hear

A small, rather sedate, gathering in a house in west London.Seven elderly Polish emigres - fiveBy BraidMary

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A NEW METHOD FOR OBTAINING SIGNIFICANT AVERAGE DIRECTIONAL

ABSTRACT: The Labyrinthodontidae Beds in the Holy Cross Mountains (PolandThe evolutionary trend of decreasing braiding of the channel system and

Is the Charlottenthal fan (marginal zone of the Pomeranian

10%) and Palaeozoic shales (PS ~4–10%). following the Polish count- ing standard (an association representing braided-stream channels

of Wartanian outwash near Bechatów, central Poland

The braided outwash of Wartanian age near Bechatw, central Poland, was formed synchronously by two river systems: glacier streams flowing from the

stratigraphy and palaeoenvironments in central Poland

Abstract The moraine plateau near BetchatÓw (central Poland) was incised These braided rivers formed during a period which may be directly correlated

Regional assessment of braided riverscape multi-decadal

braided pattern, where island density is low and0.4 16 7 0.6 9 8 1.1 13 13 1.0 23 southern Poland: Patterns, causes and con-

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Narew

in western Belarus and north-eastern Poland, is a tributary of the The Narew is one of Europes few braided rivers, the term relating to

plain in the Pomeranian glaciomarginal zone of NW Poland:

(Weichselian glaciation) Four assemblages of deposits filling shallow, braided-stream channels. Poland: a missing component of ice-contact

BRAIDED FIELD QUANTIZATION FROM QUANTUM POINCARu00c9 COVARIANCE

We demonstrate that the covariance of the algebra of quantum NC fields under quantum-deformed Poincaru00e9 symmetries implies the appearence of braided

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Narew

in western Belarus and north-eastern Poland, is a tributary of the The Narew is one of Europes few braided rivers, the term relating to

and periglacial climatic records from central Poland (

climatic records from central Poland (Bełchatów)braided deposits and the extension of aeolian mean annual air temperature lower than −4°C

Species richness and vegetation structure in different

and one on the floodplain (braided river lakes2001. Aquatic plant diversity in four river floodSE PolandThe aim of the conducted research was

in the Carpathian and peri-Carpathian landscapes (SE Poland)

preferences in the Carpathian and peri-Carpathian landscapes (SE Poland)Great changes occurred in river valleys where braided river channels changed

The role of drainage basin orography in the river channel

The role of drainage basin orography in the river channel pattern transformation during late Vistulian, Subcarpathian Oswiecim Basin, Poland on ResearchGate,

of Early Pleistocene fluvial systems in central Poland

Evolution of Early Pleistocene fluvial systems in central Poland prior to theThe younger series (Krzaki) formed mainly in a braided river setting,

system (a case study from the Sudetes Mts, SW Poland)

(Gp); thin sand zones; waning flood h4 m braided river; generally of sporadic occurrence during the 1997 and 1998 events (SW Poland)

Twentieth-century hydromorphological degradation of Polish

2017121-Polish Carpathians and those originating in the high-mountain Tatra massif the Dunajec was mostly braided, with a single-thread channel

Restoring Floodplain Forests in Europe

In braided river sys- tems, the geomorphological four essential requirements for a self-regeneratingin Poland with a view to improving river res-

Pebble fabric in braided stream deposits with examples from

(Central Sudetes, SW Poland) where the fluvial valley-floor conglomerates ofTeisseyre, A.K., 1975, Pebble fabric in braided stream deposits with

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Fluvial Processes in Braided Rivers

braided rivers, measurements of flow and sediment patterns: braided, anabranching, and single-threads impact on fluvial processes in the Polish