GEOLOGY OF DEVILS TOWER NATIONAL MONUMENT Sedimentation Pat Frolander John Aloisio Marlon Poole Lee McDowell.

Slides:



Advertisements
Similar presentations
Rocks and Minerals By:.
Advertisements

I. Minerals and Rocks. I. Minerals and Rocks.
Geology Part II The Rock Cycle Rocks: Geologic Profiles Geologic Time
Chapter 8: Rocks and Minerals
Chapter 4 - Rocks What can be learned by studying rocks…
Rocks and Fossil Fuels.
6.2 Rocks form in different ways
The Rock Cycle. THE ROCK CYCLE Rocks are constantly being formed, worn down and then formed again. This is known as the Rock Cycle It takes thousands.
Thinking about relationships among the major rock groups
By: Mika I. Gilchrist “The Rock Cycle”. A mineral is a naturally occurring, nonliving solid that has a specific chemical makeup and a crystalline,
Sedimentary Rocks Sedimentary rocks are classified by the types of sediments that make up the rock.
Rocks, Rocks, and more Rocks - Sedimentary
Sedimentary Rocks Chapter 4 Section 4.
Minerals & Rock Unit Notes 7th Grade Science
Sedimentary Rock c. Classify rocks by their process of formation.
The Rock Cycle By: Mr. Meringolo Before We Begin… Write down the following questions and answer throughout the presentation What is Sediment? What are.
Sedimentary rocks form from earlier rocks.
Chapter 3.3.  The word sedimentary comes from the latin word sedimentum, which means “settling”.  Sedimentary rocks form when sediments settle out and.
How Yosemite Valley was formed 470 million years ago to today a story of uplift, erosion, glaciation, and sedimentation.
Sedimentary Rocks are Formed from Earlier Rocks
Relative Dating and Sequencing Relative vs. Absolute Time Laws Unconformities Correlating Geologic Cross Sections.
2.4 Sedimentary Rocks.
Finding the Relative age of Rocks
8.1 The Rock Cycle 7.4.a Students know Earth processes today are similar to those that occurred in the past and slow geologic processes have large cumulative.
The Relative Age of Rocks
Locations of Rocks in Texas
The Relative Age of Rocks
Classifying Rocks Rocks are classified as either Igneous, Sedimentary, or Metamorphic.
The Rock Cycle Types of Rocks Forces that change rocks Weathering Erosion Deposition Heat and Pressure.
Rocks and Rock Cycle Mrs. Reese.
The Rock Cycle: There are many different things that can happen to a rock that will change it into a different type of rock. Ex. Weathering/erosion/compaction/cementation.
Rock Cycle Unit Vocabulary 7 th Grade Science. Weathering The breaking down of Earth’s materials by natural processes (water, wind, ice, chemicals, etc.)
The Rock Cycle.
Rocks. Three Types of rock Igneous Metamorphic Sedimentary Three totally different types of rock that all basically come from the same materials.
 The composition, structure, position and fossil content of Earth’s rocks provide information about Earth’s geologic history.  The geologic history dates.
Erosion by Glaciers. A glacier is Any large mass of ice that moves slowly over land Think of it as a moving river of ice and snow.
CHANGING EARTH Rocks, fossils, earthquakes, volcanoes.
Sedimentary Igneous Metamorphic What are minerals? Minerals are naturally occurring, nonliving substances found in Earth. They have a chemical formula,
Early Times Law of Super Position CategoriesChangesGrab.
Rock Cycle. There are three major types of rocks Igneous Sedimentary Metamorphic.
Rocks.
Sedimentary Rocks Chapter 4 Section 4. Sedimentary Rocks Sediments are loose materials like rock fragments, mineral grains, and bits of shell. Sediments.
Daily Warm-Up Exercises1 Day 12 How can sand being carried by a river eventually become sandstone? When the river slows, the sand settles and forms a layer.
Processes that Change Earth’s Surface
Rocks and The Rock Cycle. 3 Main Rock Types Igneous Sedimentary Metamorphic.
7.4.c Students know that the rock cycle includes the formation of new sediment and rocks and that rocks are often found in layers, with the oldest generally.
ROCKS, ROCKS, AND MORE ROCKS! Chapters 5 and 6 (Glencoe Earth Science)
Sedimentary Rocks 18 Starter Sedimentary Rocks 9/4/15 Application: Lab Connection Do summarize it on page 328 book. Exit: Predict the texture of an sedimentary.
By Michael Nau and Elizabeth Dorsey. Weathering vs. Erosion  Erosion involves movement and weathering does not.  Weathering is the main agent in erosion.
Rocks ROCKS Chapter 3.
 The rock cycle is a group of changes, other rocks can change to other rock.  The rocks change because of cooling, melting, weathering and.
Rock CYCLE AND Glaciation
Rock Notes- 3 types of Rock
Three Types of Rock.
4.6 billion years ago… Earth came together as a cloud of dust and gas.
SEDIMENTARY ROCKS.
Story in the Rocks By: Jana Owen, Maggie Sheehan, and Jace Johansen.
Rocks. Rock Origin Igneous Rocks - Formed from the cooling of molten magma or lava. Sedimentary Rocks- Formed from particles of other rocks or remains.
The Rock Cycle Objective: Student will identify and classify the characteristics of the rock cycle by the end of the lesson.
Rocks Part II. Three Different Types of Rocks Sedimentary – Rock produced by cemented mineral particles deposited by wind, water, ice, or chemical reactions.
The Rock Cycle Objective: Student will identify and classify the characteristics of the rock cycle by the end of the lesson.
Rocks and Rock Formation
Notes Sedimentary Rocks.
Rocks Igneous Rocks Sedimentary Rocks Metamorphic Rocks The Rock Cycle.
Chapter 2: Rocks and Minerals
Rock Cycle Review Tuesday, November 3rd 2015 Textbook pages 217 – 219.
The Rock Cycle.
Rocks and the Rock Cycle
The Rock Cycle.
Presentation transcript:

GEOLOGY OF DEVILS TOWER NATIONAL MONUMENT Sedimentation Pat Frolander John Aloisio Marlon Poole Lee McDowell

Devils Tower used to be under water in a shallow sea about 145 to 65 million years ago This was North America during the late Cretaceous time. thelivingmoon.com

Devils Tower This was the United States USGS pubs.usgs.gov

The bottoms of the ocean were covered in deep sand or mud called sediments. The Mississippi pouring sediment into the Atlantic Ocean. (ESEA esa.int)

There are 3 categories of sedimentary rocks: Clastic Organic Chemical

Clastic:Big rocks break up into small rocks And become sand, mud or silt that settle to the bottom of an ocean Which become rock again

Organic : LIMESTONE Sedimentary rock made from the shells of billions and billions of microscopic ocean organisms called plankton (foraminifera) over millions of years. Limestone can also be chemical, when the calcium from the shells becomes rock.

This is what it looks like today

Coal is an Organic rock made from ancient forests From this To this. Organic Sedimentary rock

Sediments can be Chemical As an ocean dried up, different sediments called salts were left behind. Chemical rocks include Table salt Gypsum Some Limestone

The Gypsum Springs Formation today. Gypsum is found in many places including here at Devils Tower. The White Sands in New Mexico is an example of a large deposit of gypsum. Some of our school walls are made of gypsum, it is used to make sheet rock.

Let’s review: What are the three categories of sedimentary rock? 1.Clastic, made from the smallest pieces of broken or weathered rock Includes sandstone, siltstone and shale. 2. Oganic, from ancient living things, includes coal and limestone. 3. Chemical, from when oceans dried up, includes gypsum and table salt and limestone.

Older rocks Younger rocks

When layers form, the older rocks are on the bottom, and the younger rocks are found on top. This is called the Law of Superposition. Older rocks Younger rocks

These are the sedimentary rocks you see today at Devils Tower Which rocks are the oldest? The Spearfish formation

The sea disappeared as the Rocky Mountains, with the Black Hills, began to form, about 66 – 45 Million Years Ago. (MYA) The land covering Devils Tower was no longer under water. This mountain building was called the Laramide Orogeny Devils Tower Rocky Mountains

magma

Magma

magma Future Little Missouri Buttes Future Devils Tower

Molten rock that cools and becomes hardened is called Igneous Rock.

Igneous rock that cools quickly above ground is called Extrusive. Igneous rock that cools slowly underground is called Intrusive.

This magma caused bulges to form, making dome mountains such as Bear Butte near Sturgis, S.D.

Today we see layers 18, 19 and 20. Where are layers 1 – 17?? The Sedimentary layers 1-17 on top of Devils Tower eroded away, leaving the harder, igneous rock standing. Layers 18, 19 and 20 Are now being eroded.

At the end of the last Ice Age (10,000 years ago) the outwash from the melting glaciers increased the flow of rivers throughout the North American continent. This is when geologists assume the majority of the sedimentary rocks in this area were eroded away.

Erosion Today, the Belle Fourche River does not seem large enough to wash away the vast amount of sedimentary rock eroded from above and around the Tower Have WE changed the amount of erosion at Devils Tower? Yes. Humans have dammed the Belle Fourche River, creating Keyhole Reservoir, and preventing the floods that cause the greatest amount of erosion.

It is important to note the upper portion of the tower appears more weathered with numerous vertical and horizontal cracks. Why do you think this is? Erosion (cont.) Some Geologists think that when the vertical cracks formed, the horizontal cracks also formed. Maybe the top was exposed to weathering longer than the bottom was.

Devils Tower Today