Andes Mountains Peru Chile Trench
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The resultant mountain system exhibits an extraordinary vertical differential of more than 40000 feet between the bottom of the peru chile atacama trench off the pacific coast of the continent and the peaks of the high mountains within a horizontal distance of less than 200 miles.
Andes mountains peru chile trench. The bolivian orocline is a seaward concave bending in the coast of south america and the andes mountains at about 180 s. The andes mountains of south america run parallel to the peru chile trench created as the nazca plate subducts beneath the south american plate. The peru chile trench or the atacama trench in the east pacific ocean is 8065 meters deep.
Peru chile trench also called atacama trench submarine trench in the eastern pacific ocean about 100 miles 160 km off the coast of peru and chile. It reaches a maximum depth of 26460 feet 8065 m below sea level in richards deep and is approximately 3666 miles 5900 km long. P waves change the of substances thus they can travel through solids liquids and gases.
San adreas fault the alpine fault of new xealand. Its mean width is 40 miles 64 km and it covers an expanse of some 228000 square miles 590000 square km. A brief explanation of the formation of the andes mountain range range of highs and lows.
Divisions of the andes. The formation of the andes mountains and peru chile trench resulted from the plate subducting under the south american plate. Peru chile trench andes mountains.
The strongest waves released during an earthquake are. The peruchile trench also known as the atacama trench is an oceanic trench in the eastern pacific ocean about 160 kilometres off the coast of peru and chile. The tectonic processes that created the andes have continued to the present day.
Mendocino fault eltanin fault. Mariana trench aleutian islands. Its mean width is 64 km and it covers an expanse of some 590000 km2.
Himilaya mountains the alps. From 500s several of the larger glaciers descend. The peruchile trench the forearc and the western edge of the central andean plateau delineate the dramatic bolivian orocline that defines the andean slope of southern peru northern chile and bolivia.
It is at between 4500 and 4800 m 14800 and 15700 ft in the tropical ecuadorian colombian venezuelan and northern peruvian andes rising to 48005200 m 1570017100 ft in the drier mountains of southern peru south to northern chile south to about 300s before descending to 4500 m 14760 ft on aconcagua at 320s 2000 m 6600 ft at 400s 500 m 1640 ft at 500s and only 300 m 980 ft in tierra del fuego at 550s. It reaches a maximum depth of 8065 m below sea level in richards deep and is approximately 5900 km long. You might also like.
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