Diffusion is the process of spreading new ideas from culture to culture. Examples of diffusion include the use of cars and the smelting of iron. There are five main types of diffusion they are: Expansion diffusion, Relocation diffusion, Hierarchal diffusion, Congious diffusion and Stimulus diffusion.
Immigration.
The first, and most important, part of the capital investment process is generating new ideas.
The ideas of the enlightenment
Scientists have observed the beginnings of a new ocean basin in the Afar desert in the northeast region of Ethiopia. New ocean basins are still being formed at the Mid-Ocean Ridge in the Atlantic Ocean. This process involves the formation of new basalt. The process of subduction counter-balances the aforementioned, destroying older parts of the ocean floor. This is formally known as sea-floor spreading.
New France grew slowly because of the diseases that were spreading and the harsh weather conditions.
sea-floor spreading
Yes, they were important in spreading new ideas and knowledge.
sea floor spreading
sea-floor spreading is the right
Seafloor Spreading.
new ideas spreading from one culture to aother
The process is called seafloor spreading. It occurs at mid-ocean ridges where tectonic plates move away from each other, allowing magma to rise and solidify, creating new oceanic crust.
Sea floor spreading
Seafloor spreading is the process by which new oceanic crust is formed at mid-ocean ridges. This process occurs through the upwelling of magma from the mantle to create new crust as tectonic plates move apart.
The process that forms new seafloor is called seafloor spreading. It occurs at mid-ocean ridges where new oceanic crust is created through volcanic activity. As magma rises and solidifies, it adds to the seafloor, pushing older crust away from the ridge and creating a continuous process of crust formation.
Sea floor Spreading! -Lucy laboy Thanks that really helped alot.
New seafloor is formed through a process called seafloor spreading, which occurs at mid-ocean ridges. Magma rises from the mantle and solidifies to create new crust as tectonic plates move apart. This continuous process results in the creation of new seafloor and plays a key role in plate tectonics.