The early European exploration of Australia's interior was prevented by the Western Plateau and the Great Dividing Range.
Explanation:
Australia was discovered and explored by the Europeans much latter than the other large land masses on the planet, apart from Antarctica of course. When Australia was discovered, it was not inhabited, but it was after some time when the British came that Europeans started to settle in. Australia was actually used as a prison, as it is mostly British prisoners that were brought and settled.
It was only the coastal areas that were explored and settled though, while the interior was left untouched. The reason for this were the natural obstacles, mainly the Great Dividing Range and the Western Plateau. The Great Dividing Range is a high and steep mountain range, covered with dense forest, in a roughly north-south direction, and it was extremely hard and dangerous to pass it. The Western Plateau is an enormous plateau that is mostly covered with deserts, so naturally the people avoided it.
Even nowadays, there is very big portion of Australia that is not explored and is void of humans, such as:
- Great Victoria Desert
- Great Artesian Basin
- The tropical rainforest in the northeast
- Macdonnel Ranges
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Looking down on the Earth and Moon from above the Earth's north pole, we see that its revolution is the same direction as the Earth's rotation (and also the Earth's revolution around the Sun). Therefore, at any time only one half of the Moon, the side facing the Sun, is illuminated.
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The ocean floor preserve evidence of past magnetic reversals because c) the ocean floor is uniformly old, preserving the earth's 4.6 billion history.
<h3 /><h3>What subjects need to be studied to study the earth's magnetism?</h3>
Paleomagnetism is the study of naturally occurring residual magnetism in rocks with the goal of understanding the strength and direction of the Earth's magnetic field in the geologic past and understanding the motion history of plates. Paleomagnetic fields have played a large role in confirming undersea propagation, through the discovery and understanding of seafloor anomalies. In the 1960s, geophysicists studied the magnetic properties of the ocean floor and began to discover some amazing properties.
The seabed has a system of linear magnetic anomalies in which a "band" has all its magnetic minerals oriented in the same way as the current magnetic field and the magnetic minerals in the bands alternating is oriented in the opposite direction. These bands are oriented parallel to the mid-ocean ridge system; where the ridges compensate for the transform error, the anomalies are also compensated. Symmetrical anomalies are found on either side of the ridge, and similar symmetry is found in ridges around the world.
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The correct answer is Are long, low waves out in the ocean that pile up near shore because such waves, or parts of such waves, move slower in shallower water.
Explanation:
A tsunami is a natural disaster in which waves flood the land. This phenomenon is often caused by eruptions or earthquakes in the ocean. Moreover, as a tsunami starts waves increase their longitude, indeed the longitude of waves in a tsunami can be as long as 100 kilometers. Additionally, once waves reach shallow water near the coast these increase their speed due to the friction of the seafloor, and at this point, waves pile up to form waves up to 30 meters and this causes the flood on the land and the destruction of structures. According to this, tsunamis "Are long, low waves out in the ocean that pile up near shore because such waves, or parts of such waves, move slower in shallower water."
