Answer:
GPS
Explanation:
GPS is Global positioning system , it is a satellite based navigation system which is used to identify a object on the ground or we can say its ground position . Now - a - days GPS are being used in many commercial product such as smartphones , watches , automobiles etc .
Hence , from the given options , the most appropriate is the GPS .
Answer:
c. The Torres Strait is a body of water that lies between Australia and the Melanesian island of New Guinea.
Explanation:
- The Torres Strait a strait that lies between the nations of the Australia and that of the Papua new guinea and is approximately 150 km and its name was given by the traveler Luís Torres, who passed along this strait in the 1606.
- <u>The straight link the coral sea in the east to that of the Arafura Sea to the west. The s very shallow and form at a depth of 7 to 15 m and sometimes it becomes difficult for navigation.
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- At least 274 islands the 17th of them have permanent settlements. The island varies in terms of the topographically and ecologically. And was historically formed by the inhabitants 2,500 years ago.
Answer:
Value of ∠N = 135°
Explanation:
Given that;
Quadrilateral KLMN is a parallelogram
Value of ∠K = 55°
Find:
Value of ∠N = x°
Computation:
We know that;
Quadrilateral KLMN is a parallelogram
We know that in a parallelogram, sum of co-interior angle is 180
So,
⇒ ∠K + ∠N = 180°
⇒ 55 + x = 180
⇒ x = 180 - 55
⇒ x = 135
So,
⇒ Value of x = 55
Value of ∠N = 135°
The ways are radiation , convection and conduction
Answer:
C) They are along a plate boundary in which plates are currently converging, causing uplift and steep slopes.
Explanation:
The Andean Mountain Range is by far the longest and highest mountain range in South America, and one of the largest in the world as well. Its formation is due to the convergent plate boundary between the South American plate and the Nazca plate. The Nazca plate is an oceanic plate, while the South American plate is a continental plate. The Nazca plate subducts bellow the South American plate, causing uplift in the area near the subduction zone. This has resulted in lifting up of the land, slowly creating the steep and very high Andes. The plate boundary is still active in the same way, so the process still continues.
