The fact that the global ecosystems form broad latitudinal belts is mostly because of climatic reasons. It works very simply, the shape of the Earth doesn't allow the sun to heat up the surface equally in every place, so on the equator and around it the sun heats up the Earth the most, as the latitude changes the sun rays become weaker and weaker because they fall at a smaller angle and are dispersing much more, this forms the different climatic regions on Earth thus creating different ecosystems with it, ecosystems that have their borders mostly on the lines of change in climate from one region to another, so we mostly have latitudinal belts of ecosystems.
Answer:
The correct answer is D, the Himalayan Mountains.
Explanation:
The Himalayas is a high mountain system in Asia. It is the highest mountain range on Earth and lies between the Indian subcontinent in the south and the Tibetan highlands in the north. The mountains stretch for a length of about 3000 kilometers from Pakistan to Burma and reach a width of up to 350 kilometers. In the Himalayas are ten of the fourteen highest mountains on earth, the peaks of which are more than 8000 meters high, including Mount Everest, which is 8848 m above sea level being the highest mountain on Earth. With its southern location and the Tibetan highlands rising up in the back of the Himalayas as an extensive high plateau, the Himalayas have a great influence on the climate of South and Southeast Asia.
Answer:
The intensity of sunlight decreases rapidly with depth. The depth of the water not only affects the colors of light that are noticeable underwater, it also affects the intensity, or amount of light
The meterorologist would tell the student that the northern Atlantic Ocean is far too cold to form a hurricane. Hurricanes develop in warm waters.
Answer:
1. Compaction occurs where pressure is placed on loosely packed sediment. The volume of the sediment is reduced and water is squeezed out.
2. Cementation occurs when mineral-bearing water circulates among the grains, hardens, and cements the sediment grains together. This process is most effective when lithifying sand and gravel-sized sediments.
Explanation:
