- More than 2 lakhs people are illegal migrant in Mexico.
- Illegal immigration is a crime. Maximum penalty is 6 months imprisonment with fine. In next term offense the duration of imprisonment is of 2 years.
Explanation:
Immigration means entering into a new place by leaving your own birth place. Illegal immigration refers to the intervention of people in a place without prior permission of government official. Through survey it can be counted the number of illegal immigrants. Mexico is a central American state. From where number of people rushed to north and south America.
If the immigrants catch by the police they will be punished initially for 6 months in prison with civil fine and in case of second offense they would get 2 years long imprisonment.
Pluto, it’s now a dwarf planet
Answer:
Fresh water is the very good for health.
So,Everyone should drink the fresh water.
Answer:
Extensional faulting observed in southwestern Mexico has been related to the incipient rifting of the Jalisco block from the Mexican mainland since the Pliocene. On the basis of new structural and geophysical data, we propose that (1) the continental boundaries of the Jalisco block are ancient structures reactivated since the Pliocene at a low (<1 mm/yr) rate of deformation, and (2) Pliocene-Quaternary extensional faulting at the edges of Jalisco block is a basement-controlled intraplate deformation related to plate boundary forces rather than to active continental rifting. The Jalisco block boundaries first developed in response to the uplift of the Puerto Vallarta batholith in pre-Neogene time and underwent a complex contractile deformation before the Pliocene. During Pliocene-Quaternary times north-northeast extension reactivated the northern boundary, forming the Tepic-Zacoalco rift, whereas east-southeast extension formed the northern Colima rift. South of the Colima volcano, active extension is found only west of the so-called southern Colima rift and partly reactivates old northeast-trending basement faults. The parallelism between the subducted Rivera-Cocos plate boundary zone and the eastern neotectonic boundary of the Jalisco block supports eastsoutheastward motion of the southern Mexican blocks induced by the differential motion and oblique subduction of the Cocos and Rivera plates. On the other hand, we envisage Pliocene-Quaternary extension along the northern boundary as an upper-plate response to the low convergence rate and the steep subduction angle of the Rivera plate.
