Answer:
1- Efectivamente, hoy en día nos encontramos viviendo en un mundo globalizado, ya que se trata de un sistema mundial interconectado, donde todas las sociedades y gobiernos tienen una comunicación fluida y constante entre sí en forma rápida y dinámica. Esto se ha logrado a través del desarrollo de los medios de comunicación, que permiten la conectividad a gran escala.
2- Un aspecto positivo de la globalización en mi vida personal es que el desarrollo de las comunicaciones y las tecnologías me permite poder comunicarme con personas de mi familia que viven en otro país a decenas de miles de kilómetros de distancia, con solo apretar un botón y esperar tan sólo unos pocos segundos. Es decir, la globalización acorta las distancias y reduce los tiempos, uniendo más a las personas y, por ende, a los pueblos y países.
3- Un efecto negativo de la globalización es que todos los eventos políticos y sociales que ocurren en un país tienen repercusión en los demás países. Por ejemplo, una ley en los Estados Unidos puede influir en el desarrollo del comercio en Latinoamérica, influyendo negativamente en las economías de países con menor desarrollo, pudiendo causar problemas económicos a estos.
Answer:
Ways for pollution free environment are :-
- Follow the 3 Rs ⇻ Reduce, Reuse & Recycle.
- <u>Reduce</u> the consumption of plastic products (use glass bottles, paper bags etc.)
- <u>Reuse</u> old & worn out things instead of throwing them away.
- <u>Recycle</u> your paper & plastic products.
- Use public transport, cycles or just walk ➟ this will reduce smoke & hence will reduce air pollution.
- Turn off the lights & fans when not in use ⎆ for less consumption of energy.
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# ꧁❣ RainbowSalt2²2² ࿐
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Answer:
Seafloor spreading results from intense activity in the upper mantle which cracks the crust and pushes it away.
Explanation:
Seafloor spreading is a process that was first noticed by Alfred Wegener and was used by him in his theory of plate tectonics. There are three types of plate boundaries; convergent boundary, transform boundary, and divergent boundary. The last one is the one where seafloor spreading occurs.
The convection currents in the mantle are the process that breaks up the crust and move the tectonic plates, and when there is higher activity than usual at some place it results in break up the crust of an already existing tectonic plate. Basically, magma rises at a higher rate and pushes through the crust, in this case, the oceanic crust, and it manages to gradually break through it and come out on the seafloor. By doing so, the magma and the pressure from below are pushing the two now divided parts of the plate. As the space between the two different parts becomes larger and large the density of the crust becomes smaller and smaller so more and more magma rises through. The magma quickly solidifies on the ocean floor and piles up, thus creating an underwater mountain range known as a mid-ocean ridge.
