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Earth`s Interior Introduction
Earth`s Interior Introduction

... Lithosphere – _____ and solid upper mantle  solid and rocky • Asthenosphere – soft and plastic __________mantle _______, _______, ________ rock and magma ...
Guided Reading pp
Guided Reading pp

... 1. Where and when did the island of Surtsey emerge from the ocean? 2. What do geologists do? 3. What is the science of geology and when did it begin? 4. What are the two forces that change the surface of the Earth and what does each do? 5. What are three facts about the Earth that geologists knew tw ...
Earth`s History Lesson 3: Absolute Dating
Earth`s History Lesson 3: Absolute Dating

... • When they form, minerals in igneous rocks often contain only a parent isotope and none of the daughter isotope. • This makes the isotope percentage more accurate and easier to interpret. What are some radiometric dating methods? • Scientists use many different isotopes for radiometric dating. • Th ...
RESTLESS EARTH Chapter 3: Uniformitarianism​~ A principle that
RESTLESS EARTH Chapter 3: Uniformitarianism​~ A principle that

... processes shaping the Earth today have been at work throughout Earth’s history. These changes remain ​ uniform​ or do not change over time. “The present is the key to the past” Catastrophism​ ~ A principle that states that all geologic change occurs suddenly. Mountains, canyons, and seas can be expl ...
Guided Notes for Layers of the Earth and Convection
Guided Notes for Layers of the Earth and Convection

Geo Vocab Puzzle
Geo Vocab Puzzle

... 11. state or process of a species becoming extinct, no longer existing on the Earth. 12. warm-blooded vertebrate animal of a class that is distinguished by the possession of hair or fur, the secretion of milk by females for the nourishment of the young, and the birth of live young. 17. subdivision o ...
Dual Credit Major Topics for Studying
Dual Credit Major Topics for Studying

...  Earth’s structure: Layers and properties (i.e. crust, mantle core)  Names of plates  Continental Drift  Types of volcanoes; magma types (felsic and maffic)  Features of volcanoes  Lava types  Seismic waves, earthquakes  liquefaction  2004 tsunami Rocks and Minerals  Types of rocks and roc ...
Directions: Connect the words in each sentence
Directions: Connect the words in each sentence

... Directions: Connect the words in each sentence. Always go down. ...
Ch 7 Changes to the Earth`s Surface
Ch 7 Changes to the Earth`s Surface

... •A natural land shape or feature. ...
Vocabulary Chapter 14
Vocabulary Chapter 14

... daughter isotope to determine the age of the sample ...
Earth`s Interior
Earth`s Interior

... ...
Earth`s Layers Quiz Study Guide
Earth`s Layers Quiz Study Guide

... What is the asthenosphere and lithosphere?  Where are they located?  (Add them in a  different color to the diagram in #1)  ...
Video Review
Video Review

... 1. The Earth has four layers. Color the layers of the Earth and the key. ...
Earth`s 4.6 billion years crustal history
Earth`s 4.6 billion years crustal history

... Uncovering 4.6 billion years of the earth’s history Rock specimens collected in geological field surveys between Enderby Land to the east and central Dronning Maud Land to the west are subjected to radiometric age determination using a secondary ion mass spectrometer (SHRIMP). Based on these studies, ...
G2 - Igneous processes summary
G2 - Igneous processes summary

... The S-Wave shadow zone is found between what angles? ….............................................. ...
Journal #23 - Mrs. Dawson`s Classroom
Journal #23 - Mrs. Dawson`s Classroom

... can act like natural clocks.  Atoms of the same element that have different numbers of neutrons called isotopes.  Radioactive isotopes have nuclei that emit particles and energy at a constant rate regardless of surrounding conditions. ...
Unit 3 Vocabulary
Unit 3 Vocabulary

Name: 7th Grade Science Earth History Test Review Be able to
Name: 7th Grade Science Earth History Test Review Be able to

... Principle of Uniformitarianism Relative Dating Principles such as -superposition -cross cutting relationships What are ___________ and what causes_________? (Put the terms below in the blank spaces). Faults Ridge/Rise Rifts Trenches Subduction Zone Compression Tension ...
The Origin of Earth
The Origin of Earth

... 5 billion years ago a cloud of gas and dust at least 10 billion kilometres in diameter rotated slowly in space. As time passed the cloud shrank under its own gravity. Most of the material condensed at the center. The compression made the interior so hot that fusion began and the core of the cloud fo ...
The Origin of the Earth The earth, then, grew
The Origin of the Earth The earth, then, grew

... Thus, the earth cooled to a semi-solid state fairly quickly. ...
GEO Evolution Vocab
GEO Evolution Vocab

... 5. Half-Life – the amount of time required for half of the radioactive material to decay in an item 6. Geology – the study of Earth’s history, processes, and structures 7. Geologic time scale – a timeline that organizes major events in the Earth’s history 8. Fossil – the preserved remains or evidenc ...
The Earth`s Formation
The Earth`s Formation

... The Earth’s Formation Physical and chemical processes change our planet everyday Earth as we know it is the result of events that happened ______________________ The most widely accepted model of the formation of the solar system is called the ____________________ According to scientists, the Earth ...
How the Earth was Made
How the Earth was Made

... Roberts Science ...
Ch9
Ch9

... Comets delivered the volatiles (primarily water) to the inner planets some 4 billion years ago, just after the formation of the solar system. ...
Volcanoes and earthquakes
Volcanoes and earthquakes

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Age of the Earth



The age of the Earth is 4.54 ± 0.05 billion years (4.54 × 109 years ± 1%). This age is based on evidence from radiometric age dating of meteorite material and is consistent with the radiometric ages of the oldest-known terrestrial and lunar samples.Following the development of radiometric age dating in the early 20th century, measurements of lead in uranium-rich minerals showed that some were in excess of a billion years old.The oldest such minerals analyzed to date—small crystals of zircon from the Jack Hills of Western Australia—are at least 4.404 billion years old. Comparing the mass and luminosity of the Sun to those of other stars, it appears that the Solar System cannot be much older than those rocks. Calcium-aluminium-rich inclusions – the oldest known solid constituents within meteorites that are formed within the Solar System – are 4.567 billion years old, giving an age for the solar system and an upper limit for the age of Earth.It is hypothesised that the accretion of Earth began soon after the formation of the calcium-aluminium-rich inclusions and the meteorites. Because the exact amount of time this accretion process took is not yet known, and the predictions from different accretion models range from a few millions up to about 100 million years, the exact age of Earth is difficult to determine. It is also difficult to determine the exact age of the oldest rocks on Earth, exposed at the surface, as they are aggregates of minerals of possibly different ages.
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