Answer:
<u>1. c. Peruvian coast, 2. c. Asia, 3. c. Paris, 4. Andes</u>
Explanation:
- Peru is located on the western coast of South America and faces the pacific ocean and located in the southern hemisphere it shares the longest border with brazil. Having a total area of 1,285,215.6 km square.
- Due to the latitude, mountain ranges and topography variations and the two oceanic currents like the Humboldt and El Niño which bring a diverse tropical climate of wt and dry spells to this region thus experiences a drought type conditions of the coasts of Peru.
- Places on earth most likely to encounter the trade winds are in Asia as these winds are moving in an east to west direction following the earth equatorial region, i.e 30 degrees North and South.
- To get the shortest flight from Los Angles to Moscow the plane would have to land in Paris as to refuel and thus making it the shortest flight by less than half-hour.
- Andes mountain runs parallel through the south American north to south borders.
her is this from google
"A system of temporary reference points established in the field allows users to move freely within the study area without losing the geo-referencing. It allows the user to perform the mapping of trees, deadwood, transects, repeated measurements and data verification."
<span>When new clay sediment is deposited on top of old beach material, it's known as.C. transgression.This is because the clay would have to come from sea inundating the beach ie rising and depositing the clay on the old beach. The sea rising could be from say tectonic movement or from glaciers melting but before glacial rebound.</span>
The sediments located in Heinrich layers contain almost exclusively<u> </u><u>ice</u><u>-</u><u>rafted</u><u> </u><u>detritus</u><u>, known as </u><u>IRD</u><u>.</u>
Heinrich layers are layers of sediment in the North Atlantic. These sediments have consist of high amounts of debris in Foraminiferida shells brought by ice. This composition explains how these layers function as a historical record of major ice releases.
These layers are formed from huge releases of ice of the Hudson Strait ice stream. The North Atlantic cores of sediment found in these layers are badly sorted and lack almost any foraminifera, being composed of primarily ice-rafted detritus (IRD).
These IRDs are described as sediments of no particular size that are carried by floating ice until they are introduced into the water and mix into the environment. This Ice carries debris located within it in the way a raft would carry a person, by allowing it to float on the surface of the water
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The answer is between 14% and 23.1%
