<u>Answer:
</u>
The process of thick sediment layers to "accumulate" along the "boundaries of continental and oceanic plates" is called Subduction.
<u>Explanation:
</u>
- During a marine transgression, sea level raises high compared to land level resulting in floods. These are triggered during climate changes, ice-age, isostatic movements.
- Subduction occurs at the tectonic plates where one plate is moves under another forcing to sink into Earth’s mantle due to the gravitational force.
- The plates are continental and oceanic in the zone of lithosphere. The rate of subduction is usually seven to 8 centimetres per year.
- Marine regressions are opposite to transgressions where sea levels fall compared to land levels.
- Glaciation is the interval of time within an ice-age. The current glacier period is of Holocene.
La respuesta correcta para esta pregunta abierta es la siguiente.
Las características de estos instrumentos son los siguientes.
El mapa, es la representación gráfica pero más sencilla de un lugar. Podríamos decir que es la descripción simplificada de un sitio, que incluye información métrica. El mapa es el documento básico que usamos para localizar un territorio determinado.
Las cartas sirven a la Geografía representando escalas con mayor detalle. Esto las diferencia de los mapas. En las cartas se pueden representar relieves más finos, incluyendo curvaturas.
Los planos son una herramienta muy útil en la cartografía porque son representaciones o descripciones que ayudan a la Geografía a describir extensiones de territorios a pequeñas escala.
En el caso del globo terráqueo, éste básicamente es usado por los profesores en las escuelas como un respaldo académico, cuyo objeto es enseñarle a los estudiantes las características generales de nuestro planeta. Es una manera lúdica y participativa de enseñar las curvatura de la tierra, los nombres de los continentes, los océanos, entre otras cosas.
Answer:
A landfill is the answer to the question
1. My predictions about the changes in sea level have been relatively close to the actual rise of the sea waters, though it has been different than the general predictions of the numerous models of the countries. The predictions that I have made about the rise of the sea level have been based on the rate of melting of the polar ice, but also on the isostatic rebound that occurs because of it, and the influence that the greenhouse gasses have on the global temperature. The estimates that I made were showing a rise of only few centimeters, unlike the several meters predicted by most of the models. The closest model to what I have predicted is the Russian model, which is very different than the others.
2. The sea level variations are not very easy to predict, nor do they have any particular cycle that is repeating on approximately the same time. There are numerous factors that influence the variations of the sea level, such as the global temperature, with higher temperature meaning higher sea levels, and lower temperature meaning lower sea levels. The isostatic rebound of the continental land masses should also be taken in consideration, as the continents lift up when they don't have pressure on top of them from the ice, and sink down when they do have large ice masses on them, thus it can influence where the water can penetrate and where it can't. The position of the landmasses, composition of the atmosphere, as well as the geological activities, all have big influence on the variations of the sea levels, be it going up or down.
