Gemrock and Meteor Hunting Afton Canyon
//////////////////////////////////Gemrock Hunting Barstow CA. Area////////////////////////////////
Visit Volcano Live - John Seach @ www.volcanolive.com
Layered Earth For Educators "now accepting pre-orders for The Layered Earth"!
Layered Earth integrates your Earth Science curriculum with the latest technology to prepare your students for the skills they'll need in the 21st Century. The dynamic environment, through step-by-step computer explorations, activities and resources, you''ll guide your students through a geological journey that will rock their world. Show them tectonic plate boundaries, mountain ranges, volcanoes, earthquakes, mineral resources.
Club Space Rock Meteorites and Meteorite Hunting:
Club Space Rock is the 21st-Century's best forum for learning about, talking about, buying, selling, and trading meteorites. Meet scientists and academics, professional meteorite hunters, dealers, accomplished collectors, science writers, and enthusiasts. CSR is moderated by a volunteer staff of meteorite professionals.
I have visited Afton Canyon many times, and each time there are new things to see and discover, if you are hunting Gemrock or Meteorites or just taking in Nature and enjoying the quiet and Natural Beauty . Take your hammer and metal detector. Respect Nature and check local codes.
Below: How do scientists determine the age of dinosaur bones and rocks?
Afton Canyon Area: Click on Image takes you to BLM.gov Afton Canyon Site, Below some of the minerals and gem-rock found at Afton Canyon
The Chart Below is the reverse side of the Elements Chart to the right!
Click on the Chart Below to Display Larger Image
How do scientists determine the age of dinosaur bones or rocks?
When paleontologist Mary Schweitzer found soft tissue in a Tyrannosaurus rex fossil, her discovery raised an obvious question -- how the tissue could have survived so long? The bone was 68 million years old, and conventional wisdom about fossilization is that all soft tissue, from blood to brains, decomposes. Only hard parts, like bones and teeth, can become fossils. But for some people, the discovery raised a different question. How do scientists know the bones are really 68 million years old? Today's knowledge of fossil ages comes primarily from radiometric dating, also known as radioactive dating. Radiometric dating relies on the properties of isotopes.
These are chemical elements, like carbon or uranium, that are identical except for one key feature -- the number of neutrons in their nucleus. usually, atoms have an equal number of protons and neutrons. If there are too many or too few neutrons, the atom is unstable, and it sheds particles until its nucleus reaches a stable state. Think of the nucleus as a pyramid of building blocks. If you try to add extra blocks to the sides pyramid, they may stay put for a while, but they'll eventually fall away.
The same is true if you take a block away from one of the pyramid's sides, making the rest unstable. Eventually, some of the blocks can fall away, leaving a smaller, more stable structure. The result is like a radioactive clock that ticks away as unstable isotopes decay into stable ones. You can't predict when a specific unstable atom, or parent, will decay into a stable atom, or daughter. But you can predict how long it will take a large group of atoms to decay. The element's half-life is the amount of time it takes for half the parent atoms in a sample to become daughters.
To read the time on this radioactive clock, scientists use a device called a mass spectrometer to measure the number of parent and daughter atoms. The ratio of parents to daughters can tell the researcher how old the specimen is. The more parent isotopes there are -- and the fewer daughter isotopes -- the younger the sample. Once all the parents have become daughters, there's no more basis for comparison between the two isotopes. Scientists can't tell whether the clock ran down a few days or millions of years ago. This means that isotopes with a short half-life won't work to date dinosaur bones.
The short half-life is only part of the problem when dating dinosaur bones -- researchers also have to find enough of the parent and daughter atoms to measure. Read on to see what it takes to date a fossil and what volcanic ash has to do with it. The most widely known form of radiometric dating is carbon-14 dating. This is what rchaeologists use to determine the age of human-made artifacts. But carbon-14 dating won't work on dinosaur bones. The half-life of carbon-14 is only 5,730 years, so carbon-14 dating is only effective on that are less than 50,000 years old. Dinosaur bones, on the other hand, are millions of years old -- some fossils are billions of years old. To determine the ages of these specimens, scientists need an isotope with a very long half-life. Some of the isotopes used for this purpose are uranium-238, uranium-235 and potassium-40, each of which has a half-life of more than a million years.
Unfortunately, these elements don't exist in dinosaur fossils themselves. Each of them typically exists in igneous rock, or rock made from cooled magma. Fossils, however, form in sedimentary rock -- sediment quickly covers a dinosaur's body, and the sediment and the bones gradually turn into rock. But this sediment doesn't typically include the necessary isotopes in measurable amounts. Fossils can't form in the igneous rock that usually does contain the isotopes. The extreme temperatures of the magma would just destroy the bones. So to determine the age of sedimentary rock layers, researchers first have to find neighboring layers of Earth that include igneous rock, such as volcanic ash. These layers are like bookends -- they give a beginning and an end to the period of time when the sedimentary rock formed. By using radiometric dating to determine the age of igneous brackets, researchers can accurately determine the age of the sedimentary layers between them.
Using the basic ideas of bracketing and radiometric dating, researchers have determined the age of rock layers all over the world. This information has also helped determine the age of the Earth itself. While the oldest known rocks on Earth are about 3.5 billion years old, researchers have found zircon crystals that are 4.3 billion years old [source: USGS]. Based on the analysis scientists estimate that the Earth itself is about 4.5 billion years old. In addition, the oldest known moon rocks are 4.5 billion years old. Since the moon and the Earth probably formed at the same time, this supports the current idea of the Earth's age.
FOR ADDITIONAL INFORMATION: