The correct answer to this is Option B) The French
Explanation:
Canada has long been associated with Anglo-sphere and it is true that Canada was once part of the British Empire. Till today, the head of the State is actually the Queen of England.
However, a large part of the country, and more specifically Quebec, is French speaking and was once a very powerful French colony in North America.
To date, the people are proud of their French heritage, speaking the language and passing it down to their children.
They easily form the last population group in the country after the British.
It takes about 365and 1/4 days
The geography<span> of </span>Australia<span> encompasses a wide variety of </span>biogeographic<span> regions being the world's smallest </span>continent<span> but the sixth-largest country in the world. </span>The three main geographical regions of Australia are the Western Plateau<span> ,</span>Central Lowlands<span>, </span>Great Dividing Range.
The picture is basically not necessary here, what the question is asking is : why do we have different time and different time zones?
Our time is divided into 24 hours, so you could ask: what happens every 24 hours? the answer is: the Earth rotates around its axis. So, the Earth motion responsible for this is its rotation around its axis.
Answer:
Seafloor spreading results from intense activity in the upper mantle which cracks the crust and pushes it away.
Explanation:
Seafloor spreading is a process that was first noticed by Alfred Wegener and was used by him in his theory of plate tectonics. There are three types of plate boundaries; convergent boundary, transform boundary, and divergent boundary. The last one is the one where seafloor spreading occurs.
The convection currents in the mantle are the process that breaks up the crust and move the tectonic plates, and when there is higher activity than usual at some place it results in break up the crust of an already existing tectonic plate. Basically, magma rises at a higher rate and pushes through the crust, in this case, the oceanic crust, and it manages to gradually break through it and come out on the seafloor. By doing so, the magma and the pressure from below are pushing the two now divided parts of the plate. As the space between the two different parts becomes larger and large the density of the crust becomes smaller and smaller so more and more magma rises through. The magma quickly solidifies on the ocean floor and piles up, thus creating an underwater mountain range known as a mid-ocean ridge.