Geography is the study of places and the relationships between people and their environments.
Answer:
3/32
Explanation:
Since she is putting all of the lipsticks back in the kit, that means she will always have the same "denominator" for all the probabilities.
The equation would look something like this: 2/8 * 3/8 = 6/64 = 3/32
Water leaves a lake through the ground. "Ground water is recharged from rain water and snowmelt or from water that leaks through the bottom of some lakes and rivers," - Google
Sorry if my answer was incorrect.
Answer:
Most of Latin America is located in a Tropical zone that receives the Sun's direct rays yearly.
Explanation:
Latin America, as a region, has almost exclusively tropical types of climates, with Truly Cold climates lacking from the region. The closest that climates get to truly cold types are the highest parts of the Andes and the southernmost part of the region in Patagonia and Tierra del Fuego, but none of them have polar-type characteristics all year round.
This climate situation in Latin America is due to its position relative to the Equator. The Equator passes through the widest part of the region, and the vast majority of the territory north and south falls into the tropical realm, and this is also helped by the fact that north and south of the Equator the territory shrinks and the influence of the ocean is greater. The majority of the region has a tropical wet climate, savanna-like grasslands, and tropical deserts.
The lithosphere, which is the rigid outermost shell of a planet (the crust and upper mantle), is broken up into tectonic plates. The Earth's lithosphere is composed of seven or eight major plates (depending on how they are defined) and many minor plates. Where the plates meet, their relative motion determines the type of boundary: convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The relative movement of the plates typically ranges from zero to 100 mm annually.[2]
Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction carries plates into the mantle; the material lost is roughly balanced by the formation of new (oceanic) crust along divergent margins by seafloor spreading. In this way, the total surface of the lithosphere remains the same. This prediction of plate tectonics is also referred to as the conveyor belt principle. Earlier theories, since disproven, proposed gradual shrinking (contraction) or gradual expansion of the globe.[3]
Tectonic plates are able to move because the Earth's lithosphere has greater strength than the underlying asthenosphere. Lateral density variations in the mantle result in convection. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge (due to variations in topography and density of the crust, which result in differences in gravitational forces) and drag, with downward suction, at the subduction zones. Another explanation lies in the different forces generated by tidal forces of the Sun and Moon. The relative importance of each of these factors and their relationship to each other is unclear, and still the subject of much debate.
