Meddelanden, Issues 181-183; Issues 185-194 |
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Page 64
... rise of 22 cm was recorded at Bastedalen , and about the same fall in Jönkö- ping . A comparison between the mean wind velocity needed for such a wind effect and the wind records ( cf. Fig . 17 ) also makes it proba- ble that much ...
... rise of 22 cm was recorded at Bastedalen , and about the same fall in Jönkö- ping . A comparison between the mean wind velocity needed for such a wind effect and the wind records ( cf. Fig . 17 ) also makes it proba- ble that much ...
Page 78
... rise in water level will be higher in the former areas . Currents induced by waves in shallow water Mass transport by wave motion and return flow The wave motion involves a certain transporta- tion of water mass ( equation 19 ) , and by ...
... rise in water level will be higher in the former areas . Currents induced by waves in shallow water Mass transport by wave motion and return flow The wave motion involves a certain transporta- tion of water mass ( equation 19 ) , and by ...
Page 184
... rise to new surveys , was meant to gather all land belonging to one owner into one coherent area . The Storskifte of the areas studied took place during 1788-1818 , and the Laga skifte during 1839-72 . Since the middle of the 19th ...
... rise to new surveys , was meant to gather all land belonging to one owner into one coherent area . The Storskifte of the areas studied took place during 1788-1818 , and the Laga skifte during 1839-72 . Since the middle of the 19th ...
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abrasion antal antalet åren året Baltic Ice Lake beach bedrock Befordrad godsmängd beträffande bilar bilarna bottom boulders cliff deposits depth diagram direction distribution drift emellertid erosion fetch fjärrtrafiken följande för fördelning fordon fordonen foreset bed framgår från genom glacial glacifluvial godsmängden grain granite Gränna gravel Huskvarna Jönköping Karlsborg kartan körsträcka låg Lake Vättern län landet länsgrupp lastbil lastbilar ligger longshore drift lorries m/sec material maximum miljoner moraine morphology Motala bay motsvarande mudflows något nearshore Nilsson nivå northern omfattning orientation ovan particles pebbles redovisas relativt retreat ridge rock Rosenlund samples sand sediments shore processes shoreline slide slope solifluction southern steep Stockholm stora större strata submergence surface swash tabell talus tion tonkm totala trafik trafiken transport transportarbetet transporterna undersökning uppgick uppgifter varved viktklasser visar Visingsö Visingsö island vissa water level weathering wind velocity yrkesmässig trafik