La respuesta correcta para esta pregunta correcta es la siguiente.
A pesar de que no se incluyeron opciones o incisos para responder, podemos comentar lo siguiente.
¿Quién decide qué fuentes y voces quedarán grabadas en la conciencia colectiva como parte de la historia?
Por su puesto que no es ninguna persona en particular, aunque comúnmente se dice que "los ganadores son los que escriben la historia."
Existe un concepto entre los historiadores que se llama "la memoria colectiva" o la "conciencia colectiva." Es precisamente este concepto el que define lo que permanece en la memoria histórica de las personas después de un acontecimiento.
Este concepto es el resultado de las memorias y recuerdos compartidos de uno o varios grupos sociales, que al final resultan ser las creencias compartidas que se quedan como el sello característico de un evento histórico en particular, y es el que trasciende al paso del tiempo.
Answer:which all people had freedom of speech and of religion, and freedom from want and fear.
Explanation:
Isaiah Bird is described as being "A Wrestler with No Legs and No Excuses".
Answer:
The AOC (Articles of Confederation) gave the state government more power then the national government because the founding fathers were afriad that the federal goverment would become a tyranny, like Great Britian. The federal goverment didn't have the power to request troops from the states so the US military relied on volunteers, which there were few of. The state militaries didn't send any troops so the US was unable to repond. The AOC existed for the first 5 years but then they had another constituional convention in which they overturned the AOC and drafted the constituion we have today.
Answer:
decrease in size
Explanation:
An ocean surrounded by many trenches may "decrease in size."
This is evident in the formation and process of subduction and sea-floor spreading, which has a great impact on how the oceans form in terms of size and shape.
According to research, it is believed that the sizes of Earths oceans are defined by the speed at which new crust is being developed, right from the mid-ocean ridges, and the speed at which old crust is being swept off at deep-ocean trenches
