Two forces that change coastal landforms are erosion, which is the wearing away of rock and soil by natural elements such as water and wind, and deposition, which is the process of sediment being laid down in a new location. These forces can shape coastlines through processes such as wave action, tides, and longshore drift.
Spits develop through the deposition of sediment by longshore drift, which is the movement of sediment along the shoreline caused by waves and currents. Over time, this sediment accumulates and extends outward into the water, forming a narrow, elongated strip of land that is typically oriented in the direction of the prevailing waves and currents. Vegetation such as grasses and shrubs can then colonize the spit and help to stabilize it.
The two processes that contribute to the growth of continents over time are accretion, where new landmasses are added to existing continents through tectonic activity, and magmatism, where volcanic activity generates new crust that can add to the size of continents. These processes can lead to the gradual expansion of continents over geological timescales.
Deforestation, which reduces the amount of carbon dioxide absorbed from the atmosphere, and volcanic eruptions, which release greenhouse gases and aerosols into the atmosphere, are two natural processes that also contribute to climate change.
Longshore is part of a map pack containing three maps that are not out yet. The mythic maps, Assembly, Sandbox and Orbital have come out recently but that was only one half. They are available for 800 Microsoft points on Xbox live. I have heard that longshore and the other two maps are supposed to come out Autumn this year.
There are two syllables. Drift-ing.
Spits and barrier islands are two depositional shoreline features created when longshore currents deposit sand. Spits are elongated sandbars that extend from the coast into open water, while barrier islands are long, narrow offshore deposits of sand running parallel to the shore. Both features are formed by the gradual accumulation of sand carried by longshore currents along coastlines.
The two main processes that heat Earth's core are radioactive decay of elements such as uranium, thorium, and potassium, and residual heat leftover from the planet's formation 4.5 billion years ago. These processes contribute to the high temperatures at the core, keeping it molten.
(1) melting and solidification of magma
The two types of glacial drift are till, which is unsorted sediment deposited directly by the ice, and stratified drift, which is sorted sediment deposited by glacial meltwater.
Two things that supports the continental drift theory are; 1. Fossil. 2. Continent Shapes.
The two processes that work together to make soil are weathering, which breaks down rocks into smaller particles, and organic matter decomposition, which involves the breakdown of plant and animal material by microorganisms. These processes contribute to the formation of soil by creating a mixture of mineral particles, organic matter, water, and air.