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Grand Canyon National Park

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Eileen Szychowski: Expanding Access at Grand Canyon
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50 Nifty Finds #28: Shuttering in the Cold
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Pillow Basalts
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Phenology and Climate Change: Understanding Nature’s Language through Data and Community Science
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Smallmouth Bass: Not a Small Threat to the Grand Canyon
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Notes from the Deep - Hiker Reflections from Havasupai Gardens — BTS Podcast 28
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50 Nifty Finds #35: On the Same Track
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Population Viability Analysis
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In spite of programs to encourage hiring of individuals with disabilities, it was often others’ misconceptions or discomfort that prevented women with disabilities from getting National Park Service (NPS) jobs. Those hired in the 1970s and early 1980s brought diverse skillsets and new perspectives t
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Three Parks, One Vital Ecosystem
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Data Publication Brief - Aquatic Macroinvertebrates and Upland Vegetation/Soils
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Vishnu Basement Rocks
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Geologic Timescale, Geologic Dating Techniques, and Numeric Ages
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Numeric Ages of Grand Canyon Rocks
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Significant unconformities, or gaps in the rock record that represent periods of missing time, are present between each of Grand Canyon’s three sets of rocks.
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Telling time at Grand Canyon
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The Grand Canyon Supergroup is a thick sequence of mostly sedimentary rocks deposited during the Proterozoic (between 729 and 1255 million years ago) and exposed in places in the eastern part of Grand Canyon.
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Grand Canyon’s Three Sets of Rocks
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Grand Canyon is one of the most superlative geologic locales in the world with a rock record spanning approximately one third of the planet’s history and important records of the Proterozoic Eon and Paleozoic Era.
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The Layered Paleozoic Rocks are the nearly horizontal sedimentary units exposed in the upper portion of Grand Canyon’s rock walls. They were deposited during the Paleozoic Era between about 270 and 510 million years ago.