The Sea-coast: (1) Destruction (2) Littoral Drift (3) ProtectionLongmans, Green, and Company, 1902 - 361 páginas This title deals with the effects of erosion and littoral drift on the English and continental coast-lines bordering the North Sea, and outlines protective measures including sea-walls and groynes. |
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Página 5
... shore at some past time , and where there is now no fresh source of supply . on . ( 3 ) Supplies derived from the waste of the cliffs now going The quantity of beach material contained in the first class is generally so large and covers ...
... shore at some past time , and where there is now no fresh source of supply . on . ( 3 ) Supplies derived from the waste of the cliffs now going The quantity of beach material contained in the first class is generally so large and covers ...
Página 7
... shore presents a most impressive scene , and affords a striking example of the enormous power set in motion by natural causes . Shore or littoral waves are of a different character , and to some extent are governed by different laws ...
... shore presents a most impressive scene , and affords a striking example of the enormous power set in motion by natural causes . Shore or littoral waves are of a different character , and to some extent are governed by different laws ...
Página 8
... shore , resulting in an oblique lateral movement along the shore . The water is also slightly heaped up in the centre of the channel , assuming a convex shape on the flood , and being concave on the ebb . The tidal wave , being a wave ...
... shore , resulting in an oblique lateral movement along the shore . The water is also slightly heaped up in the centre of the channel , assuming a convex shape on the flood , and being concave on the ebb . The tidal wave , being a wave ...
Página 9
... shore , but there is no forward progressive movement of the water until the margin of the shore is reached . There are two motions operating in the formation of wind waves -one horizontal , due to the wind which generates the undulation ...
... shore , but there is no forward progressive movement of the water until the margin of the shore is reached . There are two motions operating in the formation of wind waves -one horizontal , due to the wind which generates the undulation ...
Página 10
... shore , while a substance contained in the shoreward wave is thrown forward beyond the water - line , yet the ... shore would appear to warrant . This translatory movement , however , only extends for a short distance from the shore ...
... shore , while a substance contained in the shoreward wave is thrown forward beyond the water - line , yet the ... shore would appear to warrant . This translatory movement , however , only extends for a short distance from the shore ...
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The Sea-coast: 1. Destruction, 2. Littoral Drift, 3. Protection William Henry Wheeler Vista completa - 1902 |
Términos y frases comunes
12 feet 20 feet alluvium angle bank of shingle basalt beach in front beach material Blackpool boulder clay boulders Bridlington carried chalk chalk cliffs channel chert clay coast coast-line composed concrete considerable constructed Crown 8vo denudation deposited depth derived direction distance dunes east effect entrance erected erosion estuary extends face feet high Felixstowe flints flood tide foot gravel groynes harbour headland heavy gales height high tides high water Humber Illustrations inches in diameter island jetty Kilnsea land length limestone littoral drift London Clay low groynes low water marshes mile wide Morecambe Bay on-shore gales pebbles pier piles placed planking promenade protection quantity quartzite rise river rocks sand and shingle sand-hills sandstone sandy sea-wall seaward shingle and sand shingle-bank shore slope spit spring tides Spurn Point stones surface tidal timber varying wall washed waves breaking width wind Withernsea yards wide
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