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The continents erode too quickly for the Earth to be any older than million years. This is but one of the many claims that some Young-Earth Creationists have used in contention to the scientific community’s established view that the Earth is roughly 4. Backed by a handful of statistics and some overly simplistic reasoning, a number of Young-Earth Creationists argue that since the continents still have considerable elevation, the earth is relatively young. In terms of a natural clock, this claim presupposes that erosion is an irreversible process. Additionally, the claim maintains that the rate of erosion is constant and has remained constant since the formation of the Earth. By using the rate of erosion as a clock, these Young-Earth Creationists believe they have determined the origin of the earth — their initial condition — to be much younger than 4. To evaluate this claim, one must take into account the statistics which support the claim in question. For one, erosion measurements show that the continents are lowered by wind, rain, hail, waves, and living creatures’ activities Ross


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Should you date a coworker? If you still want to move forward, research shows that your intentions matter. Many companies prohibit employees from dating coworkers, vendors, customers, or suppliers, or require specific disclosures, so be sure to investigate before you start a relationship. Lots of people meet their partners at work , and yet dating someone in the office is often frowned upon.

Some companies even have explicit policies against it. So what if you and a colleague have been flirting and might want to explore a relationship? Should you steer clear? What the Experts Say There are perfectly good reasons why coworkers fall for one another , says Art Markman, a professor of psychology and marketing at the University of Texas at Austin. Research shows that we also tend to fall for people who are similar to ourselves, says Amy Nicole Baker, an associate professor of psychology at University of New Haven and author of several papers on workplace romance.

Here are some things to think about. There are also potential conflicts of interest. There are also reputational risks. So, before you jump in, check your motives and consider how others will perceive them. Having positive intentions at the start may also help guard against hurt feelings and misunderstandings should the romance eventually end.


Author contributions: P. A record of lake sediment spanning approximately years allowed us to reconstruct the long-term succession of herbicide, fungicide, and insecticide treatments in a vineyard catchment in France. This record of pesticide deposition is consistent with the historical onset and banning of these chemical substances by French and European environmental agencies.

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Water plays an important role in the transformation of the Canadian landscape by moving large amounts of soil, in the form of sediment. Sediment is eroded from the landscape, transported by river systems, and eventually deposited in a lake or the sea. The sediment cycle starts with the process of erosion , whereby particles or fragments are weathered from rock material. Action by water, wind, glaciers, and plant and animal activities all contribute to the erosion of the earth’s surface.

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We present an overview on different environmental zones within coastal areas and summarise the physical basis behind the three most important methods that are available to date Holocene coastal sediments. Besides radiocarbon and uranium series dating, Optically Stimulated Luminescence O sl has increasingly been applied for dating in coastal settings over the past decade. This is illustrated by a number of case studies showing that O sl can be applied to sediments from almost any kind of coastal environment, covering a potential dating range from some years up to several hundred thousand years.

O sl dating may hence be the method of choice for deciphering natural environmental change along coasts as well as the presence and the impact of human occupation in such areas. In addition, we briefly show how and where these dating methods could be applied to constrain the palaeo-environmental context of an archaeological site at Vohemar in north-eastern Madagascar. Comments from Tony Reimann on an earlier version are greatly appreciated.

Cliff erosion rates in Sussex have accelerated ten-fold in the past 200 years

Patrick J. Applegate, Richard B. Cosmogenic exposure dating has sometimes been used to identify moraines associated with short-lived climatic events, such as the Younger Dryas Here we point out two remaining challenges in using exposure dating to identify moraines produced by abrupt climate changes. Specifically, 1 a commonly applied sampling criterion likely yields incorrect exposure dates at some sites, and 2 geomorphic processes may introduce bias into presently accepted nuclide production rate estimates.

We fit a geomorphic process model that treats both moraine degradation and boulder erosion to collections of exposure dates from two moraines that were deposited within a few thousand years of the Younger Dryas.

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From November to February , our team is studying how rocks alter and erode in one of the most extreme environments on the planet—Antarctica. Attaching the sensors that will help us study erosion rates required vacuum grease, patience, and a lot of masking tape. After bad weather and a busy week of packing and preparation, the team is finally ready to strike out on its own in the coldest, driest, and windiest place on the planet.

A team of scientists is measuring rock breakdown in the coldest, driest, and windiest place on the planet.

We also use cosmogenic nuclides to measure how fast landscapes erode in wet and dry climate zones, respectively (for example in the Atacama desert).

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Directions: Three buttons in the lower right allow you to control the interplay between two geologic processes on a planetary surface. The processes of impact cratering and erosion are the focus of this simulation. The counters in the upper right display the passage of time. The upper readout displays the time since the simulation began or since the RESET button was pressed.

The lower readout displays the age of the surface indicated by the arrow pointer.

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The visible products of weathering and erosion are the unconsolidated materials that we find around us on slopes, beneath glaciers, in stream valleys, on beaches, and in deserts. The loose collection of material is referred to as sediment , and the individual pieces that make it up are called clasts. Clasts can be of any size: sand-sized and smaller in which case they might be referred to as particles or grains , or larger than a house.

Clasts can range widely in size and shape Figure 8. If and when deposits like these are turned into sedimentary rocks, the mineralogy and textures of these rocks will vary significantly. Importantly, when we describe sedimentary rocks that formed millions of years in the past, we can study the mineralogy and textures to make inferences about the conditions that existed during the deposition of the sediment, and the later burial and formation of sedimentary rock.

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