Day 6: Specimen Ridge Petrified Wood, Creationism, Waterfalls, Volcanism…and More.

Slides:



Advertisements
Similar presentations
The remains or evidence of a
Advertisements

Earth’s Past.
We know it’s BIG…but HOW do we know that?
FOSSILS.
Fossils Mr. Skirbst Earth Science Topic 24. Fossils The preserved remains or evidence of a living thing.
V-Shaped valleys and Interlocking Spurs.
Earth’s History in Fossils
A Trip Through Geologic Time
Slow Changes to Earth’s Surface
Sedimentary Structures Clues to depositional environments.
Fossils Fossil are the preserved remains or traces of living things. They form when living things die and are buried by sediment. They are usually.
ESS 8.4 Earth’s History.
Finding the Relative age of Rocks
Chapter 9 – 1 FOSSILS.
Rock Record Spring 2013.
Geology 12: Sedimentary Facies and Structures Facies: distinctive body of sediment Gravel On-shore fluvial Near-shore marine Off-shore marine Chert High.
Cross bedding and other indicators in sedimentary rocks What is so important about understanding how these sedimentary rocks look the way they do?
Earth’s History in Stone
Hostedby Ms. Covington Fossil Formation Clues to the Past Science Court Study of Dinosaurs
Relative Dating of Strata. Relative Dating Determining relative ages of rocks or strata compared to another rock or strata. Can say which layer is older.
Bathymetry of the Ocean Floor The ocean floor is mapped by SONAR. (Sound navigation and ranging) Depth = (time x 1500 m/sec)/2 (round trip) At 25 degrees.
Our Changing Earth The Earth is made up of different kinds of materials, including rocks. Soil, water, and the gases of the atmosphere. Soils have different.
Aim: What are the different types of rocks.
REVIEW There are 2 types of WEATHERING: 1. CHEMICAL 2. PHYSICAL
Book G Chapter 4 – Section 1
Rocks and The Rock Cycle. A. Rocks- any solid mass of mineral or mineral-like matter that occurs naturally as part of our planet B. There are 3 major.
LET’S PLAY JEOPARDY!! VocabularyD.O.S.PotluckPowerPoint How Fossils are Made $100 $200 $300 $400 $500 Final Jeopardy.
Evolution and Fossils.
Geologic Time Chapter 9.
Weathering and Erosion.
Core 1. -the center of the Earth 2 Mantle 3 the middle of the Earth made up of molten (melted) rock 4.
Chapter 11 Fossils Fossil: evidence such as the remains, imprints, or traces of once living organisms preserved in rocks Many times dead.
THIS IS With Host... Your Relative Dating Absolute Dating Radiometric Dating Fossils Vocabulary 1 Vocabulary 2.
Uncovering Earth’s Past Date: 4/3/13 p. 111 in ILL.
21.2 – Relative Age Dating How can you tell if one rock layer is older than another? How can you tell if one fossil is older than another? What is an index.
WHAT’S IN THE ROCKS!. Bell Work If you were to put the following events in to a time sequence of first to last, how would you do it? What else would you.
Absolute Age Determining How Old Geologic Features Are.
Begin Earth’s Past 3/28/12 What do you know about Fossils?
Fossils and the Rock Record
Rocks ROCKS Chapter 3.
Fossils and the Rock Record The Rock Record  Rocks record geological events and changing life forms of the past  Planet Earth was formed 4.6 billion.
Basic Geologic Principles * Principle of Superposition Principle of Original Horizontality Principle of Lateral Continuity Principle of Crosscutting Relationships.
Dating Methods / Essential Question How can scientists determine the ages of geologic material?
Fossils. Essential Question How can fossils be used to help explain what happened in the past?
2/26/13 1.List the fossils in order from the oldest to the youngest. 2.Explain why you know that is the correct order.
Relative-Age Dating. Scientists have not always thought Earth was as old as it is. James Hutton in the late 1700’s was the first geologist to think Earth.
Interpreting Landforms Landforms Created by Erosion and Deposition.
Earth’s past is revealed in rocks and fossils
Paleontology Notes Relative Age is the “age” of a rock or strata compared to the ages of other rocks or strata.
Story in the Rocks By: Jana Owen, Maggie Sheehan, and Jace Johansen.
Changes to Earth’s Surface.  The surface of the Earth is constantly changing. Some changes happen quickly and can be dangerous. Others happen so slowly,
The Rock Record Chapter 8 The earth is approximately 4.6 billion years old.
The Rock and Fossil Record
How old is old?. Earth Processes take a really, really, really (really) long time….. So, the question is – How do we know how old something is? Especially.
Evidence of a distant past Rocks provide clues to Earth’s past – some of the most obvious clues found in rocks are the remains or traces of ancient living.
A Trip Through Geologic Time
Chapter 8 The Rock Record.
A Trip Through Geologic Time
Sedimentary rocks Thursday, 15 November 2018 Learning objectives;
Aim: What are the different types of rocks.
A Trip Through Geologic Time
Chapter 8-The Rock Record Grand Canyon Video
Earth History.
A Trip Through Geologic Time
Sequencing Sedimentary Rock Layers
Geologic Time Notes By studying the characteristics of rocks and the fossils within them geologists can… interpret the environments in which the rocks.
A Trip Through Geologic Time
Fossil Sedimentary Rock Mold Cast Petrified Fossil
Chapter 17: Telling Geologic Time
The Rock Cycle Rocks vs Minerals Three Types of Rock Earth’s Layers
Presentation transcript:

Day 6: Specimen Ridge Petrified Wood, Creationism, Waterfalls, Volcanism…and More

Petrified Forest Site Up on a very steep ridge Consists of 27 layers of many buried forests Located near a glacial basin with a river flowing through it What is petrification? How is it different from fossilization and replacement?

What We Were Looking For Vertical stumps Log Alignment Sedimentary structure Types of Trees Roots, Branches, Leaves, etc. Ripple Marks and indications of flow >> These all give indications of how petrification occurred.

What we Found Vertical stumps, horizontal logs and one instance of both combined. No alignment; very few horizontal specimens MSC found; sandstone found around roots. We don’t know what types of trees were petrified. Large root system found. Some branches found. Small indications of cross-bedding. No other flow marks found. So some trees were most likely transported in a mud flow or similar event; some may not have been.

Dating Method Older Method Carbon 14 Cosmogenic Life Relative Dating

Erosion of Trees Tree on hill - outside petrified, inside eroded Outside could be mineralized first, inside more slowly; not as stable so erodes quickly –Could be from inside rotting, not completely petrified –Animals live in root holes, also help to erode Explains the erosion gradient; couplets of rings –Light ring petrified, dark not –Could be wood (50million yrs old)

Waterfalls Recall the changing nature of rivers Base level rise Base level drop

Relative Dating and the Canyon Rhyolite deposits from Dave’s speech Dike intrudes; younger than the deposit Fault line; younger than the dike Top layer usually sedimentation This allows for relative dating

Application to the Canyon Radioactive dating- two different ages on different sides of the canyon Broad valley- lava flow into it; thick Rising of river- eroded part of valley and retreated –Three river valleys New basalt and gravel flow fills in other side –Discussed possibility of two different lava flows (relatively same dates) –Glaciation on top

Hoodoos Towers of rock, usually along a riverbed Formed with a erosion-resistant rock cap Column of more erodable rock beneath it is shielded by the tough rock cap by the river Can also be eroded by wind instead of water

Merry Yellowstone Christmas!