daugava river depth
D��9)��Q��?�6IͿ��0����������c�t1G���c.hi=�+.����9�'Q�F:���I�|�Χ!�:�v��#A+r"�U�2F8��.�5���$b�n8R���"m�]�"]}����c�ɪ�NF�%;�A#e V�4�p��F��FW��UedR��0����u Ͻ�#d�;�yn$������a��K�.�h=S�R�2_���ó�O��n*�c�G�40|_X|˭Q|��i#k@�N��~������m�k�B��Fz����w`�����rF�wGP��ŗ8���nr �KaN��Q[н�� Depending on the physical and geographical conditions, a large part of the river discharge comes from either snow melt, groundwater or direct surface runoff. Determine the velocity of the boat with respect to an observer on the riverbank."

The Musa river is a tributary of the Memele river.

Coastal west basin: It includes the small river basins at the west coast with a total area of 5 100 km².

Electrotomography. Artificial groundwater recharge takes place in several well fields in Baltezers that are used for Riga city water supply. The pressure of the regional aquifer groundwater in the sandstones of the Gauja-Amata deposits of the upper Devonian balances the weight and maintains the body of the dam of Plavinas hydroelectric power station in a stable state.

It has many tributaries, the most important being the Memele, Lecava and Svete. Daugava river and dredging of sand for construction purposes from the Lielupe lower stream has essentially reduced the amount of river sediments reaching the Gulf of Riga, and caused the deficit of sediment output feeding the foreshore and beaches. Definition of soil water saturation. The following rivers are tributaries to the river Daugava (from source to mouth): According to Max Vasmer's Etymological Dictionary, the toponym Dvina clearly cannot stem from a Uralic language, and it possibly comes from an Indo-European word which used to mean river or stream. The high nitrate and phosphate load of the Daugava is instrumental to the buildup of extensive phytoplankton biomass in the Baltic Sea; other European rivers contributing to such high nutrient loading of the Baltic are the Oder and Vistula Rivers. The valley was formed in the pre-Quaternary time at low standing level of the Baltic sea. Several tributaries enter the Daugava river in Latvia, including three large ones: Ogre, Aiviekste and Dubna. 0000002317 00000 n River basins and surface water resources. Random. The cascade of the Daugava hydroelectric power plants forms continuous chain of reservoirs throughout the lower stream of the Daugava river, a substantial portion of the which is located along the buried preglacial palaeovally which depth in some places is more than 150 meters. FAA��Dz�X��4ˁӐ��q �f�f��� e�#�&���{�د00�*\ �j�R�h6�c��}A�aCcH/@� Z�r� endstream endobj 100 0 obj 353 endobj 87 0 obj << /Type /Page /Parent 80 0 R /Resources 88 0 R /Contents 92 0 R /MediaBox [ 0 0 595 842 ] /CropBox [ 0 0 595 842 ] /Rotate 0 >> endobj 88 0 obj << /ProcSet [ /PDF /Text /ImageC ] /Font << /TT2 89 0 R /TT4 94 0 R >> /XObject << /Im1 95 0 R /Im2 97 0 R /Im3 98 0 R >> /ExtGState << /GS1 96 0 R >> /ColorSpace << /Cs5 90 0 R >> >> endobj 89 0 obj << /Type /Font /Subtype /TrueType /FirstChar 32 /LastChar 150 /Widths [ 352 0 0 0 0 1076 727 0 454 454 0 818 364 454 364 454 636 636 636 636 636 636 636 636 636 636 454 454 0 818 0 0 1000 684 686 698 771 632 575 775 751 421 455 693 557 843 748 787 603 787 695 684 616 732 684 989 0 615 685 0 0 0 0 0 0 601 623 521 623 596 352 623 633 274 344 592 274 973 633 607 623 623 427 521 394 633 592 818 592 592 525 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 269 269 0 0 0 636 ] /Encoding /WinAnsiEncoding /BaseFont /Verdana /FontDescriptor 91 0 R >> endobj 90 0 obj [ /CalRGB << /WhitePoint [ 0.9505 1 1.089 ] /Gamma [ 2.22221 2.22221 2.22221 ] /Matrix [ 0.4124 0.2126 0.0193 0.3576 0.71519 0.1192 0.1805 0.0722 0.9505 ] >> ] endobj 91 0 obj << /Type /FontDescriptor /Ascent 1005 /CapHeight 734 /Descent -209 /Flags 32 /FontBBox [ -50 -207 1447 1000 ] /FontName /Verdana /ItalicAngle 0 /StemV 96 /XHeight 546 >> endobj 92 0 obj << /Length 1259 /Filter /FlateDecode >> stream 3 Floating docks up to 255 M LOA X 36 M BM.

The Rezekne and Pededze rivers are two important tributaries of the Aiviekste river.

The pressure of the regional aquifer groundwater in the sandstones of the Gauja-Amata deposits of the upper Devonian balances the weight and maintains the body of the dam of Plavinas hydroelectric power station in a stable state. Reservoir of Riga Hydropower station (Riga Hydroelectric Power Plant). It is a right tributary of the river Daugava. 0000001356 00000 n …

Inverted vertical seismic profiling.

The major rivers are Daugava, Lielupe, Gauja, Venta, and Salaca. There are about 2 250 lakes with a total area of about 850 km², most of them being small lakes with more than 10 000 lakes having a surface area of less than 1 ha (LEGMA; 2005).

The cascade of the Daugava hydroelectric power plants forms continuous chain of reservoirs throughout the lower stream of the Daugava river, a substantial portion of the which is located along the buried preglacial palaeovally which depth in some places is more than 150 meters.

Bedrock and moraine surface depth determination.

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