True. but actually there is more than one in each school especially in altrentive schools
Answer : B. dissipation.
The third stage in the development of a full tropical cyclone is the dissipation stage together with the formative and mature stage. In the formative stage, moist air moves upward causing rainfall and the circulation of the air. The cyclonic rotation is produced as more moist air are lifted. The mature stage is characterized by the increased wind speed and the sudden drop of the pressure while in the dissipation stage, the cyclone has gone weaker.
Well.. There's like a mountain and you can fly in an airplane there. <span />
The correct answer is - B. Slope of the land.
The watersheds are defined by the slopes. They can be small, medium sized, or very large. All parts of the land on planet Earth belong to one watershed or another.
The watersheds have boundaries, and those boundaries are along the highest points of the mountains or the hills. In most cases, one of the slopes of the mountain or hill is in one watershed, while the other one is in another watershed.
The water from the watershed goes into a single place as its final destination. The water can run down the slope on the ground after a heavy rainfall, get into smaller streams and rivers, get directly into a bigger river, but in the end all of that water will get to the biggest water body in the watershed.
This is the Kelvin scale - it's essentially the same as the Celsius (that is, one degree of Celsius is equivalent to one degree Kelvin, and the same cannot be said about Fahrenheit).
In Celcius the absolute zero is equivalent to <span> −273.15 °C and in Fahrenheit it's </span><span><span>−459.67 °F.</span> </span>
