At present, nearly all of the 33 Latin American and Caribbean countries have established democratic governments.
<h3>What are the political characteristics Latin America?</h3>
Latin America encompasses a vast and very diverse area of the world. The main natural features of the region include the pampa grasslands of the southern cone, the Andean mountain range, the Amazonian rainforest, the forests and volcanoes of Central America and some of the tropical islands of the Caribbean. Latin America is politically divided into four regions North America, Central America, South America, and the Caribbean.
So we can conclude that: At present, nearly all of the 33 Latin American and Caribbean countries have established democratic governments.
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They work together by keeping it alive and not dieing
Answer:
A. humid subtropical
Explanation:
Central America has several types of climates, most of which are part of the tropical climates. In the northern part of the region there are arid and semi-arid climate types, thus it is a region dominated by deserts and chaparral. The central part, stretching like a line in the heart of the region is where the highland climate is present, as this is the part of the region that is the highest in elevation. The southern part of Mexico, and the majority of the southern half of the region are dominated by tropical wet climate types, with slight variations, as some do not have dry season at all, while some have short lasting dry seasons.
The process of erosion can best be described as the movement of weathered materials by: wind water or other natural agents.
Answer:
Q.56. True. Q. 58. U shaped. Q.59. True. Q. 60. loess Deposits.
Explanation:
Scientific evidence proves that the ice core directly record climatic data and that is hidden in their layers in the form of samples of atmospheric bubbles. Like it is in rock forms. They can found based on carbon dating.
U shaped profiles are generally found in the typical profile of canyons and valley eroded and deepened by alpine or valley glaciers. Formed due to the process of glaciation.
In response to normal folding, the Horizontal, Tensile stresses that force the rocks and elongate them can be seen in Dip-slip, Strike-slip, ring faults, etc.
Loess Deposit is a fine-grained material that has been transported and deposited by winds action coming from the glacial outwash plains. Deposits include silt, sand and clays, muds residues of the glacial valleys.