Aug 08, 2013 · Really, really old. “It depends on what you mean by dirt,” says Milan Pavich, a research geologist with the U.S. Geological Survey. “The …
North Carolina is the region. We've lost ~50 feet of topsoil in North America in the last 500 years. On average, we have 2-3 inches left. The Army has been concerned about it since the 1920s and we probably have about 50 years left. To answer your …
Mar 22, 2013 · Over time much of the place disappeared. Many cities now are on flood plains, they are only standing because people maintain them constantly. posted by freya_lamb at 1:48 PM on March 22, 2013 [ 1 favorite ]
Oct 01, 2020 · Wang Tao, one of the world’s leading desert scholars, reports that from 1950 to 1975 an average of 600 square miles turned to desert each year. By century’s end, nearly 1,400 square miles (3,600 square kilometers) were going to desert annually.
Wind and water erosion take a toll. The latter can be seen in the silting of reservoirs and in satellite photographs of muddy, silt-laden rivers flowing into the sea.
Soil erosion often results from the demand-driven expansion of cultivation onto marginal land. Over the last century or so there were massive cropland expansions in two countries—the United States and the Soviet Union—and both ended in disaster.
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There may be no way of knowing. If the earth was not tilted on its axis at all there would be no seasons.
Let's also assume that the continental crust is on average 30 km thick. Let's not worry about density. The dirt layer then forms 1/30,000 of the crust and would have a mass of 7.24×10^17 kg. That's on the order of 0.00001% of the mass of the earth. 9.
Sinkholes are caused by any physical process that can hollow out a space underground. Underground streams can erode dirt and rock until a hollow space forms underground. Magma near volcanoes can move away and leave a void as it moves away. Acid rain can eat away at rock over millennia to form a cave underground.
Soil is generally made of 45% inorganic matter (rocks, minerals), 5% organic matter (decomposing leaves, manure, etc.), and 50% pore spaces containing water or air.
All rocks originated as igneous (volcanic) rock. Some of the igneous rocks are broken down, form layers, and are cemented with pressure or chemicals to form sedimentary rocks (sandstone, shale, limestone, etc.). Some igneous rocks are altered to form metamorphic rocks such as slate, marble, and gneiss.
It takes hundreds to thousands of years to form an inch of topsoil. Photo: NRCS. A: We say that it takes 500 to thousands of years to create an inch of topsoil. The reason is that soil is often derived from rock. The rock has to be broken into small pieces first.
The rock has to be broken into small pieces first. This happens by physical weathering: things like freezing and thawing in colder climates, and chemical weathering in warmer climates. Once cracks form in the rock and plants can take hold, the plants continue to break the rock into smaller pieces by root action and start to add organic matter.
Thanks, Karl! Great question. The answer is yes, microbes break down plant material into organic matter that can eventually become part of the soil. This is a great idea for a blog post, and we’ll put it on our list! Thanks for reading!
A landmark study on the topic by Donald Davis and his team of researchers from the University of Texas (UT) at Austin’s Department of Chemistry and Biochemistry was published in December 2004 in the Journal of the American College of Nutrition.
It would be overkill to say that the carrot you eat today has very little nutrition in it—especially compared to some of the other less healthy foods you likely also eat—but it is true that fruits and vegetables grown decades ago were much richer in vitamins and minerals than the varieties most of us get today.
The Tragedy of the Commons. You might have heard the expression “the tragedy of the commons.”. In 1968, an article of the same title written by Garrett Hardin described how a common pasture was ruined by overgrazing. But Hardin was not the first to notice the phenomenon.
Pollution describes what happens when contaminants are introduced into an environment (water, air, land) at levels that are damaging. Environments can often sustain a limited amount of contaminants without marked change, and water, air, and soil can “heal” themselves to a certain degree. However, once contaminant levels reach a certain point, the results can be catastrophic.
The subfield of environmental sociology studies the way humans interact with their environments. This field is closely related to human ecology, which focuses on the relationship between people and their built and natural environment. This is an area that is garnering more attention as extreme weather patterns and policy battles over climate change ...
A key factor of environmental sociology is the concept of carrying capacity, which describes the maximum amount of life that can be sustained within a given area. While this concept can refer to grazing lands or to rivers, we can also apply it to the earth as a whole. Too little land for grazing means starving cattle.
Climate Change. While you might be more familiar with the phrase “global warming,” climate change is the term now used to refer to long-term shifts in temperatures due to human activity and, in particular, the release of greenhouse gases into the environment.
The planet as a whole is warming, but the term climate change acknowledges that the short-term variations in this process can include both higher and lower temperatures, despite the overarching trend toward warmth.
Pollution. Pollution describes what happens when contaminants are introduced into an environment (water, air, land) at levels that are damaging. Environments can often sustain a limited amount of contaminants without marked change, and water, air, and soil can “heal” themselves to a certain degree.