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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Resultados 6-10 de 60
Página 51
... reach 2 miles inland , and attain a height of 150 feet , the houses adjacent being rendered uninhabitable , and the channel of the river filled up for a length of 2 miles . In Cornwall , along the north - west coast , there are ...
... reach 2 miles inland , and attain a height of 150 feet , the houses adjacent being rendered uninhabitable , and the channel of the river filled up for a length of 2 miles . In Cornwall , along the north - west coast , there are ...
Página 66
... reaches the further headland before the bay tide , and , curling round , moves then in the opposite direction to that working round the shore of the indent . The drift of the shingle in the bay in this case is in opposite directions ...
... reaches the further headland before the bay tide , and , curling round , moves then in the opposite direction to that working round the shore of the indent . The drift of the shingle in the bay in this case is in opposite directions ...
Página 75
... reaches . The line of " wrack " or débris left along a sandy shore , a little above the line of high water after every tide , is corroborative of this action . The ever - varying ridge and hollow to be found on shingle - banks during ...
... reaches . The line of " wrack " or débris left along a sandy shore , a little above the line of high water after every tide , is corroborative of this action . The ever - varying ridge and hollow to be found on shingle - banks during ...
Página 76
... reach of the retiring waves and there left stranded . In addition to the movement of individual stones , the whole of the face of the bank , above the line reached by the water under the pressure of the wave , is forced upwards , and ...
... reach of the retiring waves and there left stranded . In addition to the movement of individual stones , the whole of the face of the bank , above the line reached by the water under the pressure of the wave , is forced upwards , and ...
Página 77
... reach of the falling water . Although the ebb acts for the same period on a bank as the flood , as the shingle is situated generally high up the beach , it is not able to reverse the movement of the material . The waves lack the ...
... reach of the falling water . Although the ebb acts for the same period on a bank as the flood , as the shingle is situated generally high up the beach , it is not able to reverse the movement of the material . The waves lack the ...
Otras ediciones - Ver todas
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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