Answer:
Limestone and marble can be dissolved by weak acids in rain.
Explanation:
Limestone and marble weather faster than granite because they can be dissolved by weak acids in rain.
Answer:
The migration has changed the cultural landscape of Europe and immigrant groups have challenged or been challenged by ideas of nationalism is explained below in complete explanation.
Explanation:
Individuals who migrate encounter various pressures that can influence their reasoning well being, including the suppression of cultural models, religious practices, and social support arrangements, adaptation to a new culture, and diversity in personality and thought of self. positive outcomes of Nationalism—supports a feeling of identity, joins people, develops self-esteem. negative outcomes—commences conflicting with others.
I think the city near an ocean, which is a body of water, will have cooler temperatures than an inland city as when the wind blows, due to the cool sea water, it will have a cooling effect.
Answer:
regional and contact metamorphism
Explanation:
most metamorphic rocks are the result of regional metamorphism also called dynamothermal metamorphism. These rocks were typically exposed to tectonic forces and associated high pressures and temperatures
Answer:
It helps with stratigraphic studies.
Explanation:
Bedding planes are the sheets that distinguish each successive layer of a stratified rock from its preceding layer, also known as sedimentary planes or stratification planes.
When one layer of sediment that is completely different from the former is formed or created over the old layer, bedding is said to have occured. This new layer may comprise of sand and tiny stones (called pebbles) or other sedimentary material. Because the components of the each new successive layer are totally different from the former in terms of composition, there is a marked division between each of them identifable by their quality and colur.t
The study of each of these layers to ascertain their time scale which provides basis for studies in historical geology is called stratigraphic studies.
The initial placement of strata in geologically diverse terrains is suggested in stratigraphical studies and the depositional nature of the sediment is established.
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