Difference between revisions of "Geologically Important Radioactive Elements Used for Radiometric Dating"

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== What the radiometric dating table shows ==
 
== What the radiometric dating table shows ==
 
Six parent isotopes are listed with their daughter decay products: samarium-147 (neodymium-143), rubidium-87 (strontium-87), uranium-238 (lead-206), uranium-235 (lead-207), potassium-40 (argon-40) and carbon-14 (nitrogen-14). For each, the table gives the approximate half-life, from 5730 years for carbon-14 to 106 billion years for samarium-147, the useful dating range and the materials that can be dated. Carbon-14 is useful for organic materials from about 100 to 70,000 years old, while the other isotopes date minerals and rocks as old as 4.6 billion years.
 
Six parent isotopes are listed with their daughter decay products: samarium-147 (neodymium-143), rubidium-87 (strontium-87), uranium-238 (lead-206), uranium-235 (lead-207), potassium-40 (argon-40) and carbon-14 (nitrogen-14). For each, the table gives the approximate half-life, from 5730 years for carbon-14 to 106 billion years for samarium-147, the useful dating range and the materials that can be dated. Carbon-14 is useful for organic materials from about 100 to 70,000 years old, while the other isotopes date minerals and rocks as old as 4.6 billion years.
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== Regents Exam Questions ==
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Released Regents questions that cannot be answered without this table, listed by exam. Each link opens the question with its answer key; the standard is the one the question assesses. The exams through August 2026 were given with the earlier edition of the ESSRT, which has the same table.
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| style="background-color:white;" | [[Questions:Earth-Moon History#q5|Question 35]]
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| style="background-color:white;" | [[HS-ESS1-6]]
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| style="background-color:white;" | [[Questions:Chesapeake Bay Impact Event|Chesapeake Bay Impact Event]]
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| style="background-color:white;" | [[Questions:ESS Theia and the Moon#q3|Question 3]]
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| style="background-color:white;" | [[HS-ESS1-6]]
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Latest revision as of 16:31, 25 October 2026

⇱ All Earth and Space Sciences Reference Tables (ESSRT)
← Generalized Cross Section Model of Earth's Surface and Interior Locations of Selected Hotspots →

The Geologically Important Radioactive Elements Used for Radiometric Dating table from the Reference Tables for Earth and Space Sciences (ESSRT) lists the radioactive isotopes used to find the absolute age of rocks, minerals and organic materials. It primarily supports HS-ESS1-6.

Geologically Important Radioactive Elements Used for Radiometric Dating from the Earth and Space Sciences Reference Tables (ESSRT): table of six parent isotopes with their daughter decay products, approximate half-lives, useful dating ranges and the materials that can be dated

What the radiometric dating table shows

Six parent isotopes are listed with their daughter decay products: samarium-147 (neodymium-143), rubidium-87 (strontium-87), uranium-238 (lead-206), uranium-235 (lead-207), potassium-40 (argon-40) and carbon-14 (nitrogen-14). For each, the table gives the approximate half-life, from 5730 years for carbon-14 to 106 billion years for samarium-147, the useful dating range and the materials that can be dated. Carbon-14 is useful for organic materials from about 100 to 70,000 years old, while the other isotopes date minerals and rocks as old as 4.6 billion years.

Regents Exam Questions

Released Regents questions that cannot be answered without this table, listed by exam. Each link opens the question with its answer key; the standard is the one the question assesses. The exams through August 2026 were given with the earlier edition of the ESSRT, which has the same table.