At 67 years old, your stool could be changing due to age. If all of your stools are hard and painful you should see a gastroenterologist to see what's going on.
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∙ 9y agoNeon rocks
Yes, a rock ages at a rate of 1 year per year. ANOTHER ANSWER: Rocks don't GROW. Rocks are not 'living beings'. Rocks are not born from seeds or from 'birth'. Only 'living things' age. Rocks GET old; just like your car GETS old. It deteriorates. Rocks WEAR-AWAY when exposed to the elements.
i think rocks age becauce of the carbon inside of them.
Paleontologists use carbon dating to determine the age of rocks.
I was just wondering why in this day and age why we still have to sort out the stones and the rocks from split peas?
The age of rocks in years can be determined through techniques like radiometric dating, which involves measuring the decay of radioactive isotopes present in the rocks. By analyzing the ratio of parent isotopes to daughter isotopes in a rock sample, scientists can calculate its age with high accuracy.\common isotopes used for radiometric dating include carbon-14, potassium-argon, and uranium-lead.
age is just a number age is just a number
the ages of the rocks become increasingly older in samples obtained farther from the ridge and the younger had just come out the ridge.
Determining the order of events and the relative age of rocks by examining their positions in a sequence is called stratigraphy. This technique involves studying the layers of rock (strata) and using principles like the Law of Superposition to understand the chronological order of rock formations.
relative age
No they do not. They get their red puffy eyes from them crashing into rocks, or they're just infected. It also just depends on the age of the turtle.
The age of a rock can be determined through radiometric dating techniques, comparing the ratios of certain elements in the rock to known decay rates. By analyzing the age of the rock in relation to the ages of other rocks in the surrounding area or in similar geological contexts, scientists can establish the relative age of the rock within the geological timescale.