Answer:
Towns grew up along the rivers which had access to the sea. Rivers also provided protection from invaders. Farmers grew crops in the fertile fields that surrounded the towns. The lack of mountains was good for farming, but it made the towns easier to be invaded by enemies.
Explanation:
Well wind sheer can cut off the tops of storms. Wind sheer stops a storm and it's energy from moving upward. Because that energy is what is called latent heat and this is stopped, the storm cannot basically develop or continue on.
The volume of the cone is calculated by the formula:
V = B*H/3
r=D/2 = 6/3 = 2
where B is surface area of basis and H is height.
B is circle which fomula for surface is:
B = r^2 * pi = 3^2*3,14 = 9*3,14 = 28.26
from condition of height we write:
H = 3*D = 3*6 = 18
now volume is:
If we express all of that in equation of volume we get:
V = 1/3* 3^2*3,14*18
Answer:
Ground shaking is the primary cause of earthquake damage to man-made structures. Many factors influence the strength of earthquake shaking at a site including the earthquake's magnitude, the site's proximity to the fault, the local geology, and the soil type.When an earthquake strikes, the intensity of earthquake shaking determines the severity of damage. In turn, the main factors affecting earthquake shaking intensity are earthquake depth, proximity to the fault, the underlying soil, and building characteristics—particularly height.
Answer:
3) Zonal Flow
Explanation:
A jetstream is an area unit that typically slim bands sturdy wind within the higher levels of the atmosphere, and the wind blows from west to east in jet streams. However, the flow naturally moves to the north and south. The flow of these jetstreams follows a specific pattern between hot & cold air, which frequently occurs in winter.
Zonal flow describes how winter storms are being produced within the Northeast region. Coldfront is made during a transition zone, wherever a chilly atmospheric state replaces an atmospheric heat state. Cold air is additionally denser than hotter air. As the dense air shifts into the nice and cozy air region, it forces the friendly and comfortable atmosphere to rise ahead of the cold front quickly.
