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Telling Time at Grand Canyon National Park

A series first published by the National Park Service, in reading order.

9 페이지업데이트

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1번째 페이지CC0 1.0 (퍼블릭 도메인)
Why Grand Canyon's Rock Record Matters: Geologic Time in the Canyon Walls
2번째 페이지CC0 1.0 (퍼블릭 도메인)
The geologic timescale, relative versus numeric dating, and how radioactive decay, volcanic ash beds, cross-cutting dikes and detrital zircons put ages on Grand Canyon's rocks.
3번째 페이지CC0 1.0 (퍼블릭 도메인)
The tilted Proterozoic rocks of the Grand Canyon Supergroup, 1,255 to 729 million years old, record the assembly and breakup of the supercontinent Rodinia and some of Earth's early life.
4번째 페이지CC0 1.0 (퍼블릭 도메인)
Grand Canyon's Three Sets of Rocks: Basement, Supergroup and Layered Paleozoic
5번째 페이지CC0 1.0 (퍼블릭 도메인)
Grand Canyon's Layered Paleozoic Rocks: Ages From the Kaibab to the Tonto Group
6번째 페이지CC0 1.0 (퍼블릭 도메인)
Grand Canyon's mile of rock looks like a complete record, but more time is missing from it than preserved. The Great Unconformity, the Great Nonconformity, the Great Angular Unconformity, and what fills the gaps.
7번째 페이지CC0 1.0 (퍼블릭 도메인)
How Old Are Grand Canyon's Rocks? The Best Numeric Ages
8번째 페이지CC0 1.0 (퍼블릭 도메인)
Telling time at Grand Canyon
9번째 페이지CC0 1.0 (퍼블릭 도메인)
The Vishnu Basement Rocks at the bottom of the Grand Canyon are metamorphic and igneous rocks 1,840 to 1,375 million years old, formed as volcanic island chains collided with ancestral North America.