Scientists: Moon over the hill at 4.51 billion years old (Update)

These are K-Ar data obtained on glauconite, a potassium-bearing clay mineral that forms in some marine sediment. Woodmorappe fails to mention, however, that these data were obtained as part of a controlled experiment to test, on samples of known age, the applicability of the K-Ar method to glauconite and to illite, another clay mineral. He also neglects to mention that most of the 89 K-Ar ages reported in their study agree very well with the expected ages. Evernden and others 43 found that these clay minerals are extremely susceptible to argon loss when heated even slightly, such as occurs when sedimentary rocks are deeply buried. As a result, glauconite is used for dating only with extreme caution. The ages from the Coast Range batholith in Alaska Table 2 are referenced by Woodmorappe to a report by Lanphere and others Whereas Lanphere and his colleagues referred to these two K-Ar ages of and million years, the ages are actually from another report and were obtained from samples collected at two localities in Canada, not Alaska.

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Although they also posed new questions, the thousands of satellite photographs brought back from the Moon have permitted us to map its surface with greater accuracy than Earth could be mapped a few decades ago. We now have over kg of rocks from nine places on the Moon, rocks that have been analyzed by hundreds of scientists from many different countries. Data from a variety of experiments have revealed much about the Moon’s deep interior. As it turns out, the Moon is truly a whole new world, with rocks and surface features that provide a record of events that occurred during the first billion years of the solar system.

This record is not preserved on Earth because all rocks formed during the first million years of Earth’s history were recycled back into the interior. The importance of the Moon in studying the principles of geology is that it provides an insight into the basic mechanics of planetary evolution and events that occurred early in the solar system.

U–Th–Pb dating of lunar rocks. In the course of our research, we searched the Dho meteorite for zir U–Pb Zircon Dating of the Lunar Meteorite Dhofar S. I. Demidovaa, M. A. Nazarova, M. O and are typical of zircon from lunar granitic rocks. The composition of the products of KREEP magmatism in the source region of the.

While there are numerous natural processes that can serve as clocks, there are also many natural processes that can reset or scramble these time-dependent processes and introduce uncertainties. To try to set a reasonable bound on the age, we could presume that the Earth formed at the same time as the rest of the solar system. If the small masses that become meteorites are part of that system, then a measurement of the solidification time of those meteorites gives an estimate of the age of the Earth.

The following illustration points to a scenario for developing such an age estimate. Some of the progress in finding very old samples of rock on the Earth are summarized in the following comments. It is a compound of zirconium, silicon and oxygen which in its colorless form is used to make brilliant gems. Samples more than 3. Older ages in the neighborhood of 4. The graph below follows the treatment of Krane of Rb-Sr studies of meteorite samples from Wetherill in order to show the nature of the calculation of age from isochrons.

Considering the relative scale of nuclei and atoms , nuclei are so remote from the outer edge of the atoms that no environmental factors affect them. However, there are two obvious problems with radioactive dating for geological purposes:

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Radioactive decay[ edit ] Example of a radioactive decay chain from lead Pb to lead Pb. The final decay product, lead Pb , is stable and can no longer undergo spontaneous radioactive decay. All ordinary matter is made up of combinations of chemical elements , each with its own atomic number , indicating the number of protons in the atomic nucleus. Additionally, elements may exist in different isotopes , with each isotope of an element differing in the number of neutrons in the nucleus.

A particular isotope of a particular element is called a nuclide. Some nuclides are inherently unstable.

Age of the earth evidences for a young age of the earth and the universe. by Don Batten. Published: 4 June , last updated 13 September There are many categories of evidence for the age of the earth and the cosmos that indicate they are much younger than is generally asserted today.

Table of Contents 4. Although they also posed new questions, the thousands of satellite photographs brought back from the Moon have permitted us to map its surface with greater accuracy than Earth could be mapped a few decades ago. We now have over kg of rocks from nine places on the Moon, rocks that have been analyzed by hundreds of scientists from many different countries.

Data from a variety of experiments have revealed much about the Moon’s deep interior. As it turns out, the Moon is truly a whole new world, with rocks and surface features that provide a record of events that occurred during the first billion years of the solar system. This record is not preserved on Earth because all rocks formed during the first million years of Earth’s history were recycled back into the interior. The importance of the Moon in studying the principles of geology is that it provides an insight into the basic mechanics of planetary evolution and events that occurred early in the solar system.

Much of the knowledge we have of how planets are born and of the events that transpired during the early part of their histories has been gained from studies of the Moon. At the outset, it is important to note that we assume that the physical and chemical laws that govern nature are constant. For example, we use observations about how chemical reactions occur today, such as the combination of oxygen and hydrogen at specific temperatures and pressures to produce water, and infer that similar conditions produced the same results in the past.

This is the basic assumption of all sciences.

Clocks in the Rocks

Share 38 shares The launch will involve new challenges for China, taking off from the moon and high-speed reentry to the Earth’s atmosphere, making it ‘one of China’s most complicated and difficult space missions’, said Hu Hao, an official from China’s Lunar Exploration Programme China is aiming to send a probe to the dark side of the moon by , the first ever such trip, and hopes to put astronauts on the moon by The mission was originally designed to be uncrewed, and was set to launch in The mission will use NASA’s Orion capsule to carry up to four astronauts around the moon — the first time humans have left low orbit since It will see Nasa’s Orion, stacked on a Space Launch System rocket capable of lifting 70 metric tons will launch from a newly refurbished Kennedy Space Center in November The uncrewed Orion will travel into Distant Retrograde Orbit, breaking the distance record reached by the most remote Apollo spacecraft, and then 30, miles farther out , total miles.

The mission will last 22 days and was originally designed to test system readiness for future crewed operations.

The scientists conducted uranium-lead dating on fragments of the mineral zircon extracted from Apollo 14 lunar samples. The pieces of zircon were minuscule—no bigger than a grain of sand.

The highlands consist of the ancient lunar surface rock, anorthosite, and materials thrown out during the creation of the impact basins. Relatively young basins are shown in light colors; the oldest basins are in dark colors. Origin of Anorthosite The ancient crust of the Moon is believed to have been composed of the rock, anorthosite, a calcium-rich white rock.

This ancient crust has been smashed and redistributed by countless meteoric impacts. One explanation for the presence of anorthosite in the lunar crust is based on the assumption that the Moon was once molten. Plagioclase, a relatively light mineral, crystallized as the Moon cooled and solidified. This mineral floated toward the surface and formed anorthosite.

Heavier minerals sank and produced the denser interior of the Moon. Apollo 16 Anorthosite Anorthosite is an important rock type of the lunar highlands and probably formed the primitive lunar crust. This sample has been determined to be 4. This date corresponds to the formation of a large lunar impact basin from which the rock was thrown. Other studies indicate that the rock lay exposed on the lunar surface for 8. Shocked Rock Lunar breccias are rocks produced by the smashing, melting, and mixing of the lunar surface materials by large and small meteoric impacts.

How Old Is the Moon? Scientists Say They Finally Know

June 23rd, Author: Consequently the civilizations of the world naturally and simultaneously started developing near the rivers which initially started flowing due to the melting of glaciers near the Equator e. South India, Sri Lanka and Africa.

We have rocks from the Moon (brought back), meteorites, and rocks that we know came from Mars. We can then use radioactive age dating in order to date the ages of the surfaces (when the rocks first formed, i.e. when the lava cooled and crystallized).

Anomalies of Radiometric Dating Logic and science dictates that if something which is assumed to have a uniform rate is shown in a single example to not be uniform, the theory must be abandoned as unreliable. The previous section showed that it is entirely possible for the uniform rates of radiometric dating to be very easily changed through enviromental conditions most have been documented by secular scientists.

This section will provide 19 specific examples of this decay-rate-change having occured. Rock from a dactite lava dome at Mount St. Helens that was formed in during the eruption there was dated using the Potassium-Argon [K-Ar] method at 0. A British Engineer, Sidney P. Clementson, studied a variety of modern volcanic rock. Knowing their ages as years old, he carefully compared them to Soviet uranium tests of the same volcanic rocks.

What he found was surprising. In every instance the dates were found to be hugely incorrect with a 14 billion year the dates varied from 50 million years to Five andesite lava flows from Mt. Ngauuhoe in New Zealand. The only problem was that one was laid down , three were laid down and one in A single uranium deposit in the Colorado Caribou Mine had a radiometric error spread of million years.

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Moon rocks may have misled asteroid bombardment dating A barrage of rocks hitting the solar system 3. But some of the evidence for this proposed bombardment might be shakier than previously believed, new research suggests. Simplifications made when dating moon rocks could make it appear that asteroid and comet impacts spiked around this time even if the collision rate was actually decreasing, scientists reported in the Proceedings of the National Academies of Sciences, sciencenews.

Many scientists think that a period of relative calm after Earth formed 4. Many of the hundreds of moon rocks analyzed appear to be around 3.

Dating the Moon’s basins Over the last couple of days I have fallen down a research rabbit hole — I began with a question about clay minerals on Mars and find myself, today, writing about the history of major impact basins on the Moon.

Ancient rift valleys — closeup artist’s concept Impacts by meteorites and comets are the only abrupt geologic force acting on the Moon today, though the variation of Earth tides on the scale of the Lunar anomalistic month causes small variations in stresses. For example, the crater Copernicus , which has a depth of 3. The Apollo 17 mission landed in an area in which the material coming from the crater Tycho might have been sampled. The study of these rocks seem to indicate that this crater could have formed million years ago, though this is debatable as well.

The surface has also experienced space weathering due to high energy particles, solar wind implantation, and micrometeorite impacts. This process causes the ray systems associated with young craters to darken until it matches the albedo of the surrounding surface. However, if the composition of the ray is different from the underlying crustal materials as might occur when a “highland” ray is emplaced on the mare , the ray could be visible for much longer times.

After resumption of Lunar exploration in the s, it was discovered there are scarps across the globe that are caused by the contraction due to cooling of the Moon. Please help improve this section by adding citations to reliable sources.

Crater Face