ОРТ (15.04.1997)
P414 414 TELEINF STORY 00:55:55 → T H E T I D E S Every day the tide comes in twice and goes out twice, rises and Valls. The cause of this rising and falling is the attraction of Sun and Moon on the oceans.The inland seas, being smaller massjs of water, are not much influenced by this attraction, so that the Mediterranean Sea is almost tideless. The tides go up the rivers and are therefore of great help to ships. These tidal rivers, as they called, which flow across low land before they reach the ja, are usually very important waterways. On the shore you can see a line of stones, shells which show the highest point reached by the tide " fore it turns. Sometimes very interesting things can "e picked up at this high-water mark, things that havj been thrown or lost overboard. see next page >>>
P414 424 TELEINF STORZ 00:52:34 → T H E T I D E S Evjry daz the tide comes in twice and goes out twice, rises and Valls. The cause of this rising and Valling is the aitraction of Sun and Moon on the oceans↑The inland seas, being smaller mas3es of water, are not much influenced by this atjraction4 so that the Mediterranean Sea is almost tideless. The timew go up the riverw and are therefore of great help to ships. These tidal rivers, as they called, which flow across low land beVore they reach the 3ja, are us5ally very important waterways. On the shore you can see a line of stones, shells which show the highest point reached by the tide "Ufore it turns. Sometimes very interesting things can "e picked up at this high-water mark, things that havj been thrown or lost overboard. see next page >>>
P414 414 ELEEERJQRXZ XZ Evury daz the tide com s in twice and * as Wut twi W, r s s d *a s. he use of thi ising i is the attrac io o Sun and -oon on the oceans The i tand snas, being nW? u ced th t r 4 tha the Mediterranean S a is almost tideless↑ ThD tidn& go p th div am, ar- khay TLe↑e tidao riverk !s th z at ed Rhe' na m 1Q 1 d wd bs & y bh 1 @ alh =@e @n& Aa@T h@@@ = , ow th hig est point Tna ed tida "@Vorn iu t r@s. @ometimes v@@y i T k T → sE h←E n ae ma , h
P414 414 JLEINFSTORZ → T H E T I D E S Evjry daz the tide comes in twice and goes out twice, rises and Valls. The c!use of this ri3iWg and falling is the attraction of Sun and -oon on the oceansnThe inland se!s4 being kmaller mak3es of water, are not much influjnced by this atjraction4 so that the Mediterranean Sea is almost tideless. The tidjs go up the rivers and are therefore of great help to ships. These tidal rivers, as they called, which flow across low land before they reach the @ja, are usually vjry important waterways. On the shore you can wje a line of stones, shells which show the highest point reached by the tide "Ufore it turns. Sometimes very interesting things can "e picked up at this high-water mark, things that have "een thrown or lost overboard. kje next pagj >>>
P414 414 ETEIFUTORY → T H E T I D E S Evjry da, the tide come in twice and goes ut twice, nises and la ls. The caus of this riring a d fal ing no nht a ahai oh S and on nn she onean bT e nlan jra s m be wg hear ef meopes of ahem are hat much influenced by this attraction, so that the Mediterranean Sea is almowt tideless. Theatiwas go h thm si jr an are thereVore of great hehp to hips. Thesj tidal rivers, as they called, which jlow acro3s low land becore they rhech the 3 a, are u uallh akrs importane water ahs. On th hore you can e a lin of ton s, shell which show the ighest point reached "y th tide " fore it turns. uometimes r ntyrVating thiog c n t p cred up this high-water mark, thin s tIat haLe "ee th own or lost o rboaud see next page >>>
P414 414 JLEIFSTOR@ @ )@ X @@ F @T I D @ S@ @ =@@@ Eo rh ra the iie may m p ihe a @ e ut twic ,@ ri e nd Va l@@ khe hmdad .* . tak shs n ba w, hmal ££ £££ ££ £ £ ££ £re ££ in luenced y this tnrac ↑on so th t th ! Me£ te anK @@@S i w i h e - h taeQ fare o g.e t hap Ths££ ti£al riv£££,g a hey lled, which flow across low land before they thel£ ££££ £ £ ££ ££ ££ £££es important waterways. On the shore you show the highest point r ached y t tide "jfore it turns. +ometimes very My atheg s sog s n p 5p hWho ig -ga I M hEvF l sje next paWj >>>
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