With regard to the underwater profile of the Strait, it can be likened to a mountain, whose summit is the "saddle" (Deep 80 -
120 meters along the line joining
Ganzirri -
Punta Pezzo ), whose opposing sides have very different slopes. In this course, the fund has a median line irregular, with a maximum depth of 115 m
, which divides a Western (near
Ganzirri ) characterized by deep incisions to the east of Punta Pezzo, deeper, level. Characteristic of the northern sector of the Strait is the wide valley
Scilla , with a more profound and steep (about 200 m
). The valley begins to flatten and then become less steep towards the Tyrrhenian Sea, where is called the Basin
Palmi . The side walls of the valley, deep and steep, rising sharply, giving the cross section to form a "U". Wide and irregular depression, less incised (Valle di Messina), having also section ad "U", si riscontra nella parte meridionale. A profondità superiori ai
500 m ,
la Valle di Messina si stringe divenendo più profonda e dando origine ad un ripido
canyon sottomarino (Canyon di Messina) che si protende fino alla piana batiale dello
Ionio . Dal versante tirrenico siciliano, il fondo marino degrada lentamente fino a raggiungere i
1.000 m nell’area di
Milazzo e, per trovare la batimetrica dei
2.000 m , si deve oltrepassare l’Isola di
Stromboli . Nella parte meridionale (Mare
Ionio ), invece, the slope is very steep and not far from the "seat" you can record the depth of 500 m
between the cities of
Messina and Reggio Calabria
, beyond the widely
just over 1,200 m in South (Punta Pellaro) to reach the 2,000 m
joining the center of the ideal
Capo Taormina - Capo d'Armi
.
0 comments:
Post a Comment