Uplift occurs are converging tectonic plate boundaries and at faults with compressional forces. As two tectonic plates collide, usually, the continental plate os folded due to the pressure hence causing uplift. At reverse faults, the compression causes the earth’s crust to uplift causing a hanging wall over the footwall.
Subsidence also occurs at convergent plate boundaries. The oceanic plate is usually the one that subsidies under the tectonic plate during the collision because it is heavier. SUbsience also occurs at normal faults where the two crust moves away from each other causing a chunk of the crust to subside. The hanging wall goes lower in elevation in comparison to the footwall.
Answer:
Two genes.
There are two change gatherings:
Changes 1,2,4, and 7 didn't supplement one another, and thus are on a similar quality.
Changes 3, 5 and 6 didn't supplement one another, however supplemented with transformations 1, 2, 4, and 7. Thus, these three transformations are available together on an alternate quality.
Hello There!
If i remember correctly, the answer you are looking for is antigens.
Hope This Helps You!
Good Luck :)
- Hannah ❤
Answer: All the given symptoms describes Pertussis.
Explanation:
Pertussis can also be defined as whooping cough or 100 day cough. It is respiratory disease which is highly contagious.
it is caused by the bacteria Bordetella pertussis. It is also known to be uncontrollable as this condition does not allows the person to breathe properly.
If recognized at early stage then antimicrobial like erythromycin can be used to treat it. The symptoms of this disease lasts for a long time and is not cured easily. Its initial stage includes cold, cough and running nose, same as common cold.
El Nino is a climate cycle where the temperature of the Pacific Ocean changes because of movements of air and ocean currents. During this period, the trade winds in the south weaken, causing the warm water to move from the Western region to the Eastern region.
El Nino climate cycle begins when warm water in the western tropical Pacific Ocean shifts eastward along the equator toward the coast of South America.
Opposite of El Nino is La Niña when the waters of the tropical eastern Pacific are colder than normal and trade winds blow strongly than usual.