The deep sea.
The Cliffs of Moher are mainly composed of sandstone and shale, which were deposited around 300 million years ago during the Carboniferous period. These sediments were subsequently compressed and uplifted to form the cliffs we see today.
Sedimentary rocks are deposited in layers as strata, forming a structure called bedding. The study of sedimentary rocks and rock strata provides information about the subsurface that is useful to scientists to learn about ancient environment of area.
Glaciers from long ago shaped the landscape of Scandinavia by carving out fjords, valleys, and lakes. Their movement also deposited sediments that enriched the soil for agriculture. Today, the melting of glaciers due to climate change is contributing to rising sea levels and impacting ecosystems in Scandinavia.
Dihydrogen carbonate, H2CO3, is unstable and easily dissociates in water and carbon
Carboniferious period
The chemical formula of radium carbonate is RaCO3.
Formation of the South Dakota Badlands, or White River Badlands, began about 69 million years ago when sediments from the great sea were deposited across what is now the Great Plains. Significant erosion of the badlands began about .5 million years ago and continues today.
The process of making classic rocks involves the accumulation and lithification of sediment over time. Sediments, which can include fragments of pre-existing rocks, minerals, and organic materials, are deposited in various environments such as riverbeds, lakes, or oceans. Over time, these sediments are compacted and cemented together under pressure, forming solid rock. This geological process can take thousands to millions of years, resulting in the diverse formations we see in classic rock layers today.
Usually the Next day, so say, if you deposited a Check Today, it would show up on your Statement at 12 midnight, XD
I have no idea but need to know because "it" deposited $45 in my acct. today. Where did it come from and why?
The Canterbury Plains in New Zealand were formed by the erosion of the Southern Alps through a process called fluvial deposition, where rivers carried sediments and deposited them across the land. This geological process has been ongoing for millions of years, resulting in the flat and fertile plains that are characteristic of the region today.
No