They started using billboards i believe hope that helps
The Coriolis effect is the result of "the rotation of Earth on its axis".
<u>Answer:</u> Option B
<u>Explanation:</u>
The Coriolis force occurs either inertial or imaginary. That works on objects in movement within a reference frame that rotates in support of an inertial frame. The influence of the effect of Coriolis depends on velocity of Earth and object or substance which is being deflected by the Coriolis effect. For long distances or high velocities, Coriolis effect influence is priority.
This effect explains the wind variations in North Hemisphere to the right initiated by the earth's rotation on its axis. The Coriolis Effect accounts to the wind's circular motion around pressure systems that shift weather patterns in south-eastern USA.
It was Plessy v.
<span> Ferguson</span> that upheld the doctrine of "separate but equal" this decision was later overturned by the landmark case of Brown v. Board of Education.
Answer:
The division between accidental and deliberate voyages in the table is one of rough convenience only. A more realistic division would include a whole scale of drift voyages, vaguely deliberate voyages, off-course voyages on which the course has been recovered, accidental voyages which have ended in a successful return, etc. For this reason such details as are known of the voyages are supplied in the table so that the reader may judge for himself their category. How, for example, would he classify Nos. 37, 42, 43, and what relevance do they hold for his theory of the Polynesian dispersal? Are we to take the evidence of temporary Polynesian visits to the uninhabited islands (Nos. 135-147) as sad endings to one-way accidental voyages, when in Nos. 2, 9, 18, 30, 54, 99, we have examples of just such accidental arrivals at uninhabited islands, followed by a determined effort to return or push on?
The following table is as exhaustive as a reading of the better known works on the Pacific would allow: undoubtedly there are many more instances known by personal experience or to be found in the manuscript and newspaper sources of Pacific history. The voyages in the Polynesian area have been supplemented by some on the fringes of Western Polynesia and Melanesia from information received from Mr. Parsonson. Capt. Brett Hilder has also supplied some west-east voyages (Nos. 148-152) from his own experience. They testify partly to the invisible force of the equatorial counter-current and partly to the influence of unexpected westerlies. They may add point to the suggestion made by both Mr. Parsonson and Mr. Dening that while accidental voyages to the east have been frequent enough in the far west and equatorial zones to have occasioned the initial Polynesian dispersal, the dominant stream of accidental voyages in the Polynesian area proper has been to the west.
Explanation:
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