The highest tornade speed recorded was 302 MPH.
Mexico is a country where the social life and culture are a mixture of European and Mesoamerican traits.
Explanation:
Mexico is a country that has been part of the Spanish colonization. This has resulted in big impact by the Spanish, especially in the culture. While the Spanish imposed their own cultural traits, lot of the cultural traits of the local population shave also been kept.
The cultural landscape of Mexico nowadays is a mixture between the Spanish culture and the Mesoamerican cultures. The large cities tend to be leaning more toward the Spanish culture, while the rural areas tend to lean more toward the Mesoamerican cultures.
Unfortunately, lot of bad characteristics have been preserved from both of the different cultures that created the modern day Mexican culture. Such things have been the imposing of power over the poor and treating them as slaves, the development of local powerhouses based on criminal activities, thus the cartels, and the brutal and seeming casual murders, often of innocent people.
Some of the Mesoamerican cultures that have contributed to the Mexican culture are:
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The faults in which the hanging wall moves down relative to the footwall is called normal fault.
Explanation:
There are several types of faults based on their characteristics. One of them is the normal fault, or normal dip-slip fault. The main characteristic of this fault is that its hanging wall moves down relative to the footwall, while the footwall tends to move up relative to the hanging wall. The force that creates this type of faults is the vertical compression as the crust of Earth is lengthening.
- These faults can be found all over the world, and they are actually the most common type of faults.
- The normal dip-slip faults are bounding big portion of the mountains, as well as rift valleys.
- As these faults progress with their formation, with the footwall going up, and the hanging wall going down, the footwall becomes a hill or a mountain, while the hanging wall becomes a valley.
- The normal dip-slip faults can be found at all types of tectonic plate boundaries.
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The Maldives There it’s southwest of India and Sri Lanka
