Jewel Cave National Monument: A Guidebook
|
|
- Abel York
- 6 years ago
- Views:
Transcription
1 Jewel Cave National Monument: A Guidebook Created by: Natasha Florian, Laura Lindley, Robert Kern, and Jessica Querry University of Nebraska Lincoln / Northern Illinois University Field Course May 15th June 2nd 2006
2 The Jewel Cave guidebook has been created for the viewing of the general public. The objective of this guidebook is to explain the geology of Jewel Cave in South Dakota. This book can be used in conjunction with other resources available at Jewel Cave in order to have a better understanding of the geology, history, and importance of the cave system. Introduction: Limestone Unlike many other caves, Jewel Cave was not created or carved by underground rivers. Most of the cave was formed by acid-rich water. Between 345 and 360 million years ago, a shallow sea covered the area. Sediment and calcium carbonate-based shells accumulated at the bottom, forming limestone. Around 320 million years ago, freshwater streams deposited sediment consisting of sandstone, with a few thin beds of limestone and dolomite. Approximately 60 Sandstone million years ago, long after the sea receded for the last time, the Black Hills began to form. About 40 million years Dolomite ago, freshwater passed underground through soil that was rich in carbon dioxide and formed a weak acid known as carbonic acid. As it traveled through fractures and filled the cavities in the limestone, Jewel Cave was formed. Jewel Cave is the second longest known cave in the
3 world. When the cave was filled with water, the water began to leach the calcium out of the limestone in the walls. Eventually, the concentration of calcium ions in the water got to a point where the water could no longer dissolve any more calcium. This is called a supersaturated solution. At this point, the calcium began to precipitate out and form the crystal structures. This can be seen in the pictures of the beakers above (with c showing the precipitation). As the water drained from the cave, the pressure holding up some of the structures was removed and they fell down to the floor of the cave. The process by which crystals and rocks fall over time is known as breakdown. After this, water dripping into Jewel Cave over time created its variety of formations. Crystals of the mineral calcite, deposited from millions of droplets, make up the formations. Jewel Cave is named for its many rooms and passages that are covered Calcite crystals Stalactite
4 with jewel-like crystals, some of which sparkle like gems when illuminated. Almost every chamber of Jewel Cave has an impressive collection of calcite crystals. Where drops fall from the ceiling, stalactites form; where drops hit the floor, stalagmites grow; and where stalactites and stalagmites have merged, columns appear. Water trickling down a slanted ceiling creates translucent draperies, and water flowing over a wall leaves behind flowstone. Calcite crystals Stalagmite Jewel cave is also home to many unique formations. While these may be found off the path of the scenic tour, specimens are available in the visitor s center and can also be seen along the spelunking tour. These formations include straws, bacon strips, popcorn, and hydromagnesite balloons. The hydromagnesite balloons are only present at six locations in the world. Examples of these can be seen below.
5 Soda straw and Dog s Tooth
6 Hydromagnesite Balloon
7 Location and Logistics: Directions: Jewel Cave national monument is located 13 miles west of Custer, South Dakota. To get to the site, you will need to start from Rapid City, South Dakota or Newcastle, Wyoming and then follow the directions below: From Rapid City, SD - Take Highway 16 through Hill City to Custer. Continue on Highway 16 west 13 miles to Jewel Cave National Monument. Turn left at the sign for the visitor center. From Newcastle, WY - Take Highway 16 east and drive 24 miles to Jewel Cave National Monument. Do not turn off Hwy. 16 at the Jewel Cave National Monument's Historic Area. Continue 1 mile east to the right turn for the visitor center. For a map of the site and the trials, please see the map at the end of the section. Parking: The parking lot at the visitor center can accommodate up to 10 buses. There are also accessible ramps and sidewalks available from the parking lot. Trails and Tours: Once at Jewel Cave, there are a few different routes that can be taken. For those who would prefer to stay above ground, there are two self-guided trails at Jewel Cave National Monument and one U. S. Forest Service trail located approximately 1 mile (1.61 km) west of Jewel Cave National Monument's visitor center entrance on Highway 16. The trails are diverse: from a 1/4-mile (.4 km) to over 5.5 miles (8.9 km), from level to steep and rugged, and everything in between. There is bound to be at least one trail just right for you.
8 When venturing out please keep in mind the following trail courtesies: ~ Please stay on designated trails and don't cut switchbacks. ~ Tell someone your route and carry a first aid kit. ~ Pack out your trash and if you find trash along the trail, please pick it up. ~ Carry drinking water with you on the trail. ~ Be prepared for weather changes. ~ Please do not pick the wildflowers. ~ Natural features must remain undisturbed. ~ Watch for poison ivy, rocks, and other hazards along the trail. ~ In summer, check your body and clothing frequently for ticks. For those that would like to go into the caves, the first step is to go to the visitor s center. From there, you can decide what tour you would like to take. The Scenic Tour is offered
9 year-round and runs three to twenty-two times a day depending on the time of year (more frequent during warmer months). The Scenic Tour provides an opportunity to visit chambers decorated with calcite crystals and other speleothems, while walking on a paved trail. You will enter and leave the cave by elevator from the visitor center. This tour is considered moderately strenuous. It is a 1/2-mile loop that includes 723 stair steps scattered throughout the loop. It lasts approximately 1 hour and 20 minutes. Low-heeled, rubber-soled shoes and a light jacket or sweater are recommended for the tour. The cave temperature is 49 degrees year-round. Persons who have heart or respiratory problems, have recently been hospitalized or have a fear of heights or closedin spaces should talk with a park ranger before selecting a tour. There is a limit of 30 people on each tour. During spring and summer months, and holidays, this tour will frequently sell out. Tickets are sold on a first come, first served basis at the visitor center or by phone up to seven days in advance. For advance reservations please call , ext. 0 from 8:00 am to 4:00 pm daily. Tours can sell out at any time of the year. All tours require a minimum of 2 participants.
10 The fee is $8.00 for adults, $4.00 for youth 6-16, children 5 and under free. The Jewel Cave Discovery Tour is also available. This tour runs three to six times daily and is offered year-round. This talk is an introduction to Jewel Cave. Participants view one large room of the cave and go up and down fifteen stair steps. This talk is also handicap accessible. The fee for this tour is $4.00 for ages 17 and over and free for ages 16 and under. For the more adventurous types, there is the Spelunking Tour. With hardhat in place and headlamp turned on you are ready to experience the cave in its natural state. Feel the wind at Hurricane Corner, ascend Martha's Kettle, crawl through the Roller Coaster and squeeze into the Brain Drain. Participants scramble over cave "breakdown," chimney between cave walls, use a hand line to climb a nearly vertical wall, and belly-crawl through tight passages. The cavers visit 2/3 mile of cave, and learn about low-impact caving, caving techniques and safety. The tour lasts 3-4 hours and is extremely strenuous. Anyone having a fear of closed spaces or heights should not attempt this tour.
11 Participants must be 16 years of age and older. All participants are required to provide proof of age, upon request. A parent or legal guardian is required to sign, on the day of the tour, a waiver of responsibility for any 16 or 17-year-old participants and should remain at the monument throughout the duration of the tour. Participants must be in good physical condition and are required to pass through an 8-1/2 inch by 24-inch crawl space before beginning the tour. Refunds are not given for those visitors unable to negotiate the block. This tour is offered early June through mid-august. The monument provides a hardhat and headlamp to each participant. The participant provides: sturdy, above ankle, rubbersoled, lug-soled, lace-up boots, long pants or coveralls, and a long-sleeved shirt, a change of clothing, shoes, and a plastic bag for carrying soiled clothes and boots from the visitor center after the tour. Gloves, soft kneepads and elbow pads are required and must be provided by the participant. Clean clothes and shoes must be brought to the visitor center when you check in for the tour. Black manganese deposits encountered during this tour will permanently stain clothing and footwear.
12 Reservations are required and can be made up to one month in advance by calling , ext. 0. This tour can sell out. Tour size is limited to a minimum of 2 visitors and a maximum of 5 visitors. Tours may be canceled due to lack of the required number of participants or due to emergencies at the Monument. For more information on this tour you may call the visitor center at , ext. 0. The fee is $ Organized groups are encouraged to make arrangements for cave programs one month in advance. Advance arrangements can be made for the Scenic Tour, Discovery Program and Lantern Tour. To arrange a group tour please contact the park at least one month prior to your visit by calling , ext. 0 or by writing to Jewel Cave National Monument, Attn: Group Tour Reservations, US Hwy. 16, Bldg. B12, Custer, SD If your request is written, please include your phone number. When discussing tour arrangements with National Park Service staff, please indicate if someone in your group has special needs. You will receive written confirmation, if time allows. You must reconfirm your tour arrangement at least two days prior to your visit by phoning , ext. 0. If the tour really interests you or anyone in your group, you can do the crystal growing exercise located at the following website: growcryst.html Also see the resources section for more websites and ideas.
13 Resources: For more information on Jewel Cave National Monument, please check out the following sources. This website explains the Jewel Cave tours, activities above the cave, and facts about the cave. o Visit this website if you want to learn more about cave exploration. o For information about the cave and pictures go to this website. o For detailed information on the cave, visit this website. o For a good description of history, exploration, geology, and visitation, please visit this website. o For detailed information on visiting the cave, visit this website. o
14 Glossary: Breakdown The act or process of failing to function or continue. Calcite - The crystallized form of calcium carbonate. The main mineral which makes up speleothems. Carbonic Acid - A weak acid created by water mixing with carbon dioxide in the soil. This acid can dissolve limestone. Cave - An underground hollow, usually with an entrance in a hill or cliff. Crystal - A solid material with a regular internal arrangement of atoms. Dolomite - A magnesia-rich sedimentary rock resembling limestone. Formations - Common term for cave feature formed by minerals being deposited into a cave such as stalactites and stalagmites. Properly termed "speleothems".
15 Limestone/Pahasapa Limestone - A sedimentary rock composed mainly of calcium carbonate. Geology - The study of the structure of the earth's crust, its formation, and development of its layers. It includes the study of individual rock types and early forms of life found as fossils in rocks. National Monument - An area of scenic beauty, historical importance, or other significance set aside by a Presidential Proclamation. These areas are maintained and preserved by the Federal Government for the enjoyment of present and future generations. Sandstone - A sedimentary rock formed by the consolidation and compaction of sand and held together by a natural cement, such as silica. Speleology - The scientific study of both the physical and biological aspects of caves. Speleothem - Proper term for the secondary deposit features in a cave, such as stalactites and stalagmites, derived from the Greek word "spelaion" meaning cave and "thema" meaning deposit. Sometimes erroneously called "decorations." Supersaturated solution - Solutions containing more dissolved solute than normal at a particular temperature. References: -- National Park Service, Jewel Cave -- Jewel Cave website
LBJWC - Sinkhole Lesson
LBJWC - Sinkhole Lesson Concept Caves and sinkholes are major openings in the ground that recharge water to the Edwards Aquifer. Objective - Students will: 1) identify a sinkhole, cave, fracture, fault,
More informationMuseum of Natural History & Science Interpretation Guide for The Cavern
Museum of Natural History & Science Interpretation Guide for The Cavern A cave is a naturally occurring hole in the ground large enough to be explored by humans. Caves can be found on every continent in
More informationDraw a picture of an erupting volcano and label using the following words/phrases: magma; lava; cools slowly; cools quickly; intrusive; extrusive
Lesson 3.2a NOTES: Igneous Rocks (Unlock) Essential Question: How are igneous rocks described? Learning Target: I can describe how igneous rocks are formed and classified Igneous Rock How does igneous
More informationName: Period: Date: ID: A. Circle the choice that best completes the statement or answers the question and write the letter on the blank.
Name: Period: _ Date: _ ID: A Unit 7 Practice Circle the choice that best completes the statement or answers the question and write the letter on the blank. 1. What term describes the movement of rock
More informationLaura J. Crossey Bachelors Degree, Geology Masters Degree, Geology Ph.D., Geology
Laura J. Crossey Bachelors Degree, Geology Masters Degree, Geology Ph.D., Geology BIO Laura Crossey has been at the University of New Mexico for seventeen years where she teaches Geology and does research.
More informationSolution Processes and. Karst Topography
Solution Processes & Karst Topography Come forth into the light of things, Let Nature be your teacher. William Wordsworth 1 Solution Processes and Karst Topography The Impact of Solution Processes on the
More informationAssignment Discovery Online Curriculum. Lesson title: Unique Landforms. Grade level: 3-4. Duration: Two class periods
Assignment Discovery Online Curriculum Lesson title: Unique Landforms Grade level: 3-4 Duration: Two class periods Objectives: Students will do the following: Learn how water and erosion affect the landscape
More information8UNIT. External dynamics of the Earth. What do you remember? Key language. Content objectives
8UNIT External dynamics of the Earth What do you remember? Can you name the solids in the photograph? nd the liquid? Is the liquid moving? How does it move? What is the name of this formation of water?
More informationEarth s crust is made mostly of Igneous rocks. There are 3 main types of Sedimentary Rocks: 1. Clastic 2. Chemical 3. Organic
Sedimentary Rocks Earth s crust is made mostly of Igneous rocks. But, most rocks on Earth s s surface are Sedimentary Rocks.. (75%) Sedimentary Rocks Sedimentary rocks are rocks that are made of broken-down
More informationGEOL 110. Sedimentary Layering. Geologic Structures (faults, joints, folds), Unconformities, Karst. Sedimentary Layering 9/23/17. Geologic Structures
GEOL 110 Sedimentary Layering Geologic Structures (faults, joints, folds), Unconformities, Karst Layering = horizontal, continuous banding produced during sediment deposition Sedimentary Layering Geologic
More informationSedimentary Rocks, our most Valuable Rocks. Or, what you will probably find when you are outdoors exploring.
Sedimentary Rocks, our most Valuable Rocks Or, what you will probably find when you are outdoors exploring. Sedimentary rocks give us evidence to earth s earlier history. We look at processes happening
More informationInside and Outside Carlsbad Caverns
by ReadWorks Imagine watching hundreds of thousands of bats swirl around you, swarming to form a large, black mass that flies off into the horizon. At Carlsbad Caverns in New Mexico, this scene is a regular
More informationTest is over no later than 9:40 p.m. There are 43 questions. Each is worth points, for a total of 100 points.
Student name NOTE: Test 2 - Form B 3370:133 Section 001 SAMPLE Caves Count pages to make sure that you have all of them. Turn in this question sheet when done. Fill in all information requested on the
More informationChapter 6 Pages of Earth s Past: Sedimentary Rocks
Chapter 6 Pages of Earth s Past: Sedimentary Rocks Introduction! Drilling into the bottom of the North Sea, we encounter: " Soft mud and loose sand, silt, pebbles, and shells. Then: " Similar materials
More informationADVENTURES IN WATER DEVELOPED BY LOUISVILLE WATER COMPANY
ADVENTURES IN WATER DEVELOPED BY LOUISVILLE WATER COMPANY Tunneling for Water explains the science behind a first-of-its-kind project in the world! Louisville Water Company is the first water utility
More informationMammoth Cave National Park, Kentucky
Mammoth Cave National Park, Kentucky Objectives of Today s Lecture Refresher on Sedimentary Depositional Systems and Rock Classifications Transgressive and Regressive Marine Environments Carbonate Depositional
More informationWestern Treatment Plant (WTP)
Western Treatment Plant (WTP) Venue and Safety Information Please complete the following important actions in preparation for your tour: Read and pass on the below information to all WTP tour participants.
More informationWeek 4/5: Limestone & Rock ages
Week 4/5: Limestone & Rock ages Monday Warm Up: Write two things you still need to finish in order to be prepared for your presentation tomorrow. LT: I can make a presentation about my solution to a science
More informationCoal Miners Museum 900A Main St, Whitwell TN coalminersmuseum.com
Preserving Our Coal Mining Heritage Coal Miners Museum 900A Main St, Whitwell TN 423 658 6868 coalminersmuseum.com Tennessee has a rich and long coal mining history. Coal mining began here in small quantities
More informationErosion and Deposition
CHAPTER 3 LESSON 2 Erosion and Deposition Landforms Shaped by Water and Wind Key Concepts What are the stages of stream development? How do water erosion and deposition change Earth s surface? How do wind
More informationBats Galore! By ReadWorks
Bats Galore! Bats Galore! By ReadWorks Imagine watching hundreds of thousands of bats swirl around you, swarming to form a large, black mass that flies off into the horizon. At Carlsbad Caverns in New
More informationWhat is a water table? What is an aquifer? What is the difference between a spring and a well?
CHAPTER 11 3 Water Underground SECTION The Flow of Fresh Water BEFORE YOU READ After you read this section, you should be able to answer these questions: What is a water table? What is an aquifer? What
More informationEPS 50 Lab 4: Sedimentary Rocks
Name: EPS 50 Lab 4: Sedimentary Rocks Grotzinger and Jordan, Chapter 5 Introduction In this lab we will classify sedimentary rocks and investigate the relationship between environmental conditions and
More informationGEOMORPHOLOGY WHAT AM I EXECTED TO LEARN?
GEOMORPHOLOGY WHAT AM I EXECTED TO LEARN? Define rock. List and recognize clear examples of the three primary rocks types. Explain the difference between the three different ways sedimentary rocks are
More informationRocks. Sedimentary Rocks. Before You Read. Read to Learn
chapter 3 Rocks section 4 Sedimentary Rocks What You ll Learn how sedimentary rocks form how sedimentary rocks are classified Before You Read Imagine you are stacking slices of bread, one on top of the
More informationReservoirs and Production
Lesson Plan Page 1 Topic: Reservoirs and production Topic Overview: Porosity refers to the percentage of holes (pores) in the rock. Permeability is the ability of fluids to travel through porous rocks.
More informationInternet Interactive Rock Cycle
Internet Interactive Rock Cycle Directions: Go to the website http://www.uky.edu/as/geology/howell/goodies/elearning/module05swf.swf and answer the questions below. Part I: Igneous Rocks (click on Igneous
More informationEssentials of Geology, 11e
Essentials of Geology, 11e Groundwater Chapter 10 Instructor Jennifer Barson Spokane Falls Community College Geology 101 Stanley Hatfield Southwestern Illinois Co Jennifer Cole Northeastern University
More informationCore Curriculum/Oklahoma AIMS Education Foundation
Topic Rocks Key Question How can models, drawings, and reading passages help you understand some ways that rocks form in layers? Learning Goals Students will: model how sediment layers can form rocks,
More informationModule 10: Resources and Virginia Geology Topic 4 Content: Virginia Geology Notes
Virginia is composed of a very diverse landscape that extends from the beaches and barrier islands all of the way to the highly elevated Appalachian Plateau. Geologists have discovered ancient shallow
More informationCT Science Standard 4.3 Erosion Water has a major role in shaping the earth s surface. Trail Guides
Trail Guides We have created a set of Trail Guides for use by you and your students as you explore our galleries on your field trip. The first section consists of the trail guides with teacher notes (pages
More informationESC 1000 (Neuhoff) Assignment #2: Rocks and Tectonics
1 ESC 1000 (Neuhoff) Assignment #2: Rocks and Tectonics Name: UF ID: Assignment is due by the beginning of class on Wednesday, October 13. This assignment is worth 45 points towards your final grade. Please
More informationAbrasion: The physical weathering of rocks by particles rubbing against each other.
FOSS Earth History Course Glossary (10-4-04) Abrasion: The physical weathering of rocks by particles rubbing against each other. Absolute age: The exact age of an object (such as a rock or artifact); found
More informationSedimentary Rocks. Rocks made of bits & pieces of other rocks.
Sedimentary Rocks Rocks made of bits & pieces of other rocks. Sedimentary Rocks Igneous rocks are the most common rocks on Earth, but because most of them exist below the surface you might not have seen
More informationFamily Sleepover Survival Guide Season
Family Sleepover Survival Guide 2017-2018 Season Contents Introduction Letter... 3 Family Sleepover Refund and Cancellation Policies... 3 General Information... 4 Check-in Process... 4 Food... 4 Sleeping
More informationSedimentary Rocks. Rocks made of bits & pieces of other rocks.
Sedimentary Rocks Rocks made of bits & pieces of other rocks. Sedimentary Rocks Igneous rocks are the most common rocks on Earth, but because most of them exist below the surface you might not have seen
More informationState the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks.
Objectives State the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks. Compare three types of unconformities. Apply the law of crosscutting
More informationTHE CHANGING SURFACE OF THE EARTH
THE CHANGING SURFACE OF THE EARTH Key words Drain geological agent weathering erosion Sediment deposition transport The landscape is a consequence of the action of two types of geological processes; internal
More informationAccess Statement for Kielder Observatory
Access Statement for Kielder Observatory Introduction Kielder Observatory is a centre for outreach in astronomy located in Kielder Forest, Northumberland nestled in under the largest expanse of protected
More informationNew Rock from the rock Cycle. Copyright 2010 Ryan P. Murphy
New Rock from the rock Cycle Copyright 2010 Ryan P. Murphy Video: Sedimentary Rocks What is sediment? Sedimentary Rocks - - - - Copyright 2010 Ryan P. Murphy Sediments are compacted, cemented together
More informationSedimentary rock covers most of Earth s surface. The other two kinds of rocks that make up Earth are igneous rocks and metamorphic rocks.
Print Close Window Display: Section Full Article Sedimentary Rocks A Rocky Start Have you ever broken a rock? Every day, natural forces break rocks into smaller rocks. Forces such as wind and rushing water
More informationDavid Gold Hiking Tours
David Gold Hiking Tours Join us for a West Texas Active Adventure Tour February 14 21, 2017 Led by David Gold and Ulrike Porat The Big Bend area of West Texas is one of the most remote, and least visited
More informationSection I: Multiple Choice Select the best answer to each question. Mark your final answer on the answer sheet. (1 pt each)
Sedimentary Rocks & Surface Processes Quest Name: Earth Science 2013 Block: Date: Section I: Multiple Choice Select the best answer to each question. Mark your final answer on the answer sheet. (1 pt each)
More informationLETTER TO PARENTS SCIENCE NEWS. Dear Parents,
LETTER TO PARENTS Cut here and paste onto school letterhead before making copies. Dear Parents, SCIENCE NEWS Our class is beginning a new science unit using the FOSS Earth Materials Module. We will investigate
More informationWeather and climate. reflect. what do you think? look out!
reflect You re going on vacation in a week and you have to start thinking about what clothes you re going to pack for your trip. You ve read the weather reports for your vacation spot, but you know that
More informationVantage/Columbia Basin Field Trip
Geology 152 Name Vantage/Columbia Basin Field Trip The primary goal of this course is to help you see the Earth from a different perspective a geological one. To accomplish this goal you will be expected
More informationSedimentary Rocks - are one of the three main rock types
Today s Objective: What Makes Sedimentary Rocks Special? Sedimentary Rocks - are one of the three main rock types A sedimentary rock can form one of three ways: 1. by the deposition of the weathered remains
More informationEDUCATION PROGRAMS GUIDE
EDUCATION PROGRAMS GUIDE Inner Space Center University of Rhode Island Graduate School of Oceanography innerspacecenter.org ABOUT THE ISC The Inner Space Center (ISC) is an international leader in ocean
More informationBowen s Chemical Stability Series
Lab 5 - Identification of Sedimentary Rocks Page - Introduction Sedimentary rocks are the second great rock group. Although they make up only a small percentage of the rocks in the earth s crust (~5%)
More information1. Base your answer to the following question on The diagram below represents a part of the crystal structure of the mineral kaolinite.
1. Base your answer to the following question on The diagram below represents a part of the crystal structure of the mineral kaolinite. An arrangement of atoms such as the one shown in the diagram determines
More informationSedimentary Rocks Reading with Questions (Pg. 3-6) Scheme for Sedimentary Rock Identification Video (Mr. White s website) Questions (Pg.
Do At Least 2 Must Do All NAME: Kick Off Activity Comparing Sedimentary and Igneous Rocks (Pg. 2) The Foundation Sedimentary Rocks Reading with Questions (Pg. 3-6) Scheme for Sedimentary Rock Identification
More informationTopic 6: Weathering, Erosion and Erosional-Deposition Systems (workbook p ) Workbook Chapter 4, 5 WEATHERING
Topic 6: Weathering, Erosion and Erosional-Deposition Systems (workbook p. 95-125) Workbook Chapter 4, 5 THE BIG PICTURE: Weathering, erosion and deposition are processes that cause changes to rock material
More informationWhat is weathering and how does it change Earth s surface? Answer the question using
7 th Grade Lesson What is weathering and how does it change Earth s surface? Answer the question using the sentence frame. You have 4 minutes. Weathering is. This changes the Earth s surface because. 1
More informationThe Niagara Escarpment extends from western New York, through the GTA all the way up to Manitoulin Island and into Michigan and Wisconsin.
is southern Ontario s most prominent topographic feature, extending more than 500 kilometres from western New York, through Niagara Falls and the western part of the Greater Toronto Area (GTA), and north
More informationSedimentary Environments Chapter 8
Sedimentary Environments Chapter 8 Does not contain complete lecture notes. To be used to help organize lecture notes and home/test studies. What is a sedimentary rock? Sedimentary rocks are products of
More informationTahlequah Public Schools Inclement Weather Transportation Plan
Tahlequah Public Schools Inclement Weather Transportation Plan Inclement Weather with Ice and Snow From time to time throughout the school year, weather may force a change in the District s normal operating
More informationFocus on Fossils. Third - Fifth. Earth Science TEKS. Vocabulary
Focus on Fossils Third - Fifth Earth Science TEKS Third Grade: 3.7A Fourth Grade: 4.7B Fifth Grade: 5.7A, 5.7D Vocabulary decomposition, deposition, erosion, extinct, fossil, paleontologist, relative dating,
More informationSchool of Rock (1 hour, Then 20 Minutes Each Day for the Following Five Days)
School of Rock ( hour, Then 0 Minutes Each Day for the Following Five Days) Addresses NGSS Level of Difficulty: Grade Range: 6-8 OVERVIEW In this activity, students explore the effects of physical and
More informationEarth Science 11: Earth Materials, Sedimentary Rocks
Name: Date: Earth Science 11: Earth Materials, Sedimentary Rocks Chapter 1, pages 56 to 66 2.4: Sedimentary Rocks Sedimentary Rock Formation All sedimentary rocks form through compaction and cementation
More informationKeeping well and healthy when it is really cold
Cold Weather Plan for England 2012 Keeping well and healthy when it is really cold Easy Read version of: Cold Weather Plan for England 2012: Protecting health and reducing harm from severe cold. What
More informationDifferent Forces Act on Objects
Have you heard the story about Isaac Newton sitting under an apple tree? According to the story, an apple fell from a tree and hit him on the head. From that event, it is said that Newton discovered the
More informationField Trip 1 Tunnel Mill, Vernon, Indiana: Waldron Shale
Geol G308 Paleontology and Geology of Indiana Name: Field Trip 1 Tunnel Mill, Vernon, Indiana: Waldron Shale On this trip we will visit Tunnel Mill, which is located just south of Vernon, Indiana in the
More informationSuggested Activities Processes that Shape the Earth: Weathering and Erosion
Suggested Activities Processes that Shape the Earth: and Erosion From Harcourt Science Teacher Ed. Source (Grade Level) Title Pages Concept Harcourt Science (5) How Water Changes C4-5 Erosion Earth s Surface
More informationLesson 1 Rocks and the Rock Cycle
Lesson 1 Student Labs and Activities Page Launch Lab 8 Content Vocabulary 9 Lesson Outline 10 MiniLab 12 Content Practice A 13 Content Practice B 14 School to Home 15 Key Concept Builders 16 Enrichment
More informationIGNEOUS. What is a Rock? What is the difference between a rock and a mineral? Rocks are made up of minerals.
Name NOTES What is a Rock? o Naturally-occurring mixtures of, mineraloids, glass or organic matter. o Rocks are divided into 3 groups based on how they were formed: What is the difference between a rock
More informationPractice Test Rocks and Minerals. Name. Page 1
Name Practice Test Rocks and Minerals 1. Which rock would be the best source of the mineral garnet? A) basalt B) limestone C) schist D) slate 2. Which mineral is mined for its iron content? A) hematite
More informationChapter 14. Groundwater
Chapter 14 Groundwater Importance of groundwater! Groundwater is water found in the pores of soil and sediment, plus narrow fractures in bedrock! Groundwater is the largest reservoir of fresh water that
More informationAccess Statement for Kielder Observatory
Access Statement for Kielder Observatory Introduction Kielder Observatory is a centre for outreach in astronomy located in Kielder Forest, Northumberland nestled in under the largest expanse of protected
More informationUNIT 4 SEDIMENTARY ROCKS
UNIT 4 SEDIMENTARY ROCKS WHAT ARE SEDIMENTS Sediments are loose Earth materials (unconsolidated materials) such as sand which are transported by the action of water, wind, glacial ice and gravity. These
More informationThe physical breakdown and chemical alteration of rocks and minerals at or near Earth s surface.
The physical breakdown and chemical alteration of rocks and minerals at or near Earth s surface. The material that is chemically and mechanically weathered to yield sediment and soil. Regolith consisting
More informationMinerals and Rocks. Rocks
Minerals and Rocks Rocks What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column if you agree with the statement or a D if you
More informationChemical Sedimentary Rocks: CARBONATES a quick summary
Chemical Sedimentary Rocks: CARBONATES a quick summary Alessandro Grippo, Ph.D. What are Carbonates? Carbonate rocks are chemical sedimentary rocks composed mainly or only by carbonate minerals Carbonate
More informationChapter 9 : Rocks and Minerals
Table of Contents Chapter 9 : Rocks and Minerals Section 2: Igneous and Sedimentary Rocks Section 3: Metamorphic Rocks and the Rock Cycle Section 2 and 3: Rocks and the Rock Cycle There are 3 different
More informationTeacher Information. The Rock Snow Park. 7900B Crystal Ridge Drive Franklin, WI A Science of Tubing Physics Adventure THE ROCK SNOW PARK
Teacher Information The Rock Snow Park 7900B Crystal Ridge Drive Franklin, WI 53132 A Science of Tubing Physics Adventure THE ROCK SNOW PARK Experience our Physics Adventure at The Rock Snow Park by enrolling
More informationEcoregions Glossary. 7.8B: Changes To Texas Land Earth and Space
Ecoregions Glossary Ecoregions The term ecoregions was developed by combining the terms ecology and region. Ecology is the study of the interrelationship of organisms and their environments. The term,
More informationFrost and ice at Hallowe en Rift. Published Descent, December p Vince Simmonds
Frost and ice at Hallowe en Rift. Published Descent, December 2018. p42-43 Vince Simmonds The rift in An Unexpected Development, first descent 8 th August 2018. Photograph by Roz Simmonds Introduction
More informationCAVES CAVES BAYS BEACHES CANYONS ISLANDS LAKES MOUNTAINS PENINSULAS PLAINS VALLEYS GLACIERS HILLS. Titles in This Series. Exploring.
Caves Titles in This Series E M PL Melody S. Mis SA ROSEN / PowerKids Press ISBN 978-1-4358-2713-4 Geographical CAVES Melody S. Mis ISLANDS LAKES MOUNTAINS PENINSULAS PLAINS VALLEYS Exploring Exploring
More informationMinerals By Patti Hutchison
Minerals By Patti Hutchison 1 Minerals. They are all around us. We eat them, wear them, and build with them. What is a mineral? How are they identified? What can we do with them? 2 Earth's crust is made
More informationRocks & Minerals. Lesson 1 Properties of Minerals. What is a mineral? What is a mineral?
Rocks & Minerals What is a mineral? A mineral must have 5 specific characteristics to be considered a mineral a. b. c. d. e. Naturally occurring - formed by natural processes. Solid - must have a definite
More informationThe Rocky Road Game. Sedimentary Rock. Igneous Rock. Start. Metamorphic Rock. Finish. Zone of Transportation. Weathering Way.
Sedimentary Rock Deposition Depot Zone of Transportation Transported: Advance 3 Weathering Way The Rocky Road Game Uplift: Advance 5 Lithification Lane Crystallization Crossway Submerge Detour take the
More informationTim Carr - West Virginia University
Tim Carr - West Virginia University Exploration s Ultimate Goal is to Answer Four Questions: Where to Drill? What to Expect? How Certain? How Profitable? Location & Depth HC Volumes Chance of Success
More informationNC Earth Science Essential Standards
NC Earth Science Essential Standards EEn. 2.1 Explain how processes and forces affect the Lithosphere. EEn. 2.1.1 Explain how the rock cycle, plate tectonics, volcanoes, and earthquakes impact the Lithosphere.
More informationLab 7: Sedimentary Structures
Name: Lab 7: Sedimentary Structures Sedimentary rocks account for a negligibly small fraction of Earth s mass, yet they are commonly encountered because the processes that form them are ubiquitous in the
More informationSedimentary Rocks. All sedimentary rocks begin to form when existing rocks are broken down into sediments Sediments are mainly weathered debris
Rocks! Objectives Describe the major processes involved in the formation of sedimentary rock Distinguish between clastic sedimentary rocks and chemical sedimentary rocks Identify the features that are
More informationWalking Long Distance Trails - Generic
Company: Thistle Trekking LTD Location: UK Description of Work Activity or Area of the Workplace Assessed: Long Distance Trails Walking Long Distance Trails - Generic All RA s should be reviewed if changes
More informationPacific Northwest Rock Lab, Part II. Igneous Rocks. Name Per.
Name Per. Pacific Northwest Rock Lab, Part II After you ve classified all your rocks, place their numbers next to the names and read the information about the rock. Check the classifications here (igneous,
More informationChapter 10. Chapter Rocks and the Rock Cycle. Rocks. Section 1 Rocks and the Rock Cycle
Chapter 10 Rocks 1 Chapter 10 Section 1 Rocks and the Rock Cycle 2 10.1 Rocks and the Rock Cycle Magma is the parent material for all rocks. Once the magma cools and hardens, many changes can occur. Geology:
More informationCITY OF NEW LONDON WINTER ROAD & SIDEWALK MAINTENANCE POLICY
CITY OF NEW LONDON WINTER ROAD & SIDEWALK MAINTENANCE POLICY GENERAL The purpose of this policy is to set up acceptable procedures and policies for the winter maintenance of public areas in the City of
More informationThe Norwood Science Center. Geology (Minerals) Grade 4
The Norwood Science Center Geology (Minerals) Grade 4 Background Information: Where do rocks come from? At first you might think the answer to this question is simple. Igneous rock comes from either magma
More informationSCI-5 KES 5.7 Geology Post-test Exam not valid for Paper Pencil Test Sessions
SCI-5 KES 5.7 Geology Post-test Exam not valid for Paper Pencil Test Sessions [Exam ID:1D5NLH 1 Earth's crust is made of plates that move slowly. This movement changes the appearance of the Earth's crust
More informationBradbury Mountain, Pownal, Maine
Maine Geologic Facts and Localities August, 2008 Bradbury Mountain, Pownal, Maine 43 o 53 56.56 N, 70 o 10 45.11 W Text by Henry N. Berry IV, Department of Agriculture, Conservation & Forestry 1 Introduction
More informationThanks. You Might Also Like. I look forward helping you focus your instruction and save time prepping.
Thanks Connect Thank you for downloading my product. I truly appreciate your support and look forward to hearing your feedback. You can connect with me and find many free activities and strategies over
More information13. Sedimentary Rocks I (p )
13. Sedimentary Rocks I (p. 194-208) Sediment Deposition Weathering results in rock being broken down into smaller fragments, called regolith. This regolith is then broken down to form soil. The regolith
More informationRock Identification. invisible rhyolite andesite basalt komatiite. visible granite diorite gabbro peridotite
Rock Identification The samples in this lab are arranged into four groups: igneous, sedimentary, metamorphic, and unknown. Study the igneous, sedimentary, and metamorphic collections to get an idea of
More informationBOY SCOUTS GEOLOGY MERIT BADGE
Requirements highlighted in yellow will be covered at the club show. Merit Badge Counselors will be on-hand. Please bring your own paperwork. Children under 12 and scouts in uniform are admitted to the
More information7.5. Weathering Breaks Down Rocks
7.5 Weathering Breaks Down Rocks Preview the section and read the headings. How many types of weathering will you be learning about in this section? An old cemetery can be an interesting place to visit.
More informationTRACE FOSSIL FOSSIL ICE CORE RELATIVE DATING SUPERPOSITION ABSOLUTE DATING GEOLOGIC COLUMN UNIFORMITARIANISM HALF-LIFE RADIOACTIVE DECAY
THIS IS NOT THE SAME TEST. YOU MUST ANSWER ALL QUESTIONS. NAME: Bubble the circle below U3L1 Write the letter next to the vocab term VOCAB MATCH 1 A. O B. O C. O D. O 1 2 A. O B. O C. O D. O 2 3 A. O B.
More informationOur Planet Earth. I nteractions of Earth Systems
CHAPTER 3 LESSON 2 Our Planet Earth I nteractions of Earth Systems Key Concepts How does the water cycle show interactions of Earth systems? How does weather show interactions of Earth systems? How does
More informationTrip to National Weather Service & NASA Thursday, June 12, by Claude Cox and Mike Kees
Trip to National Weather Service & NASA Thursday, June 12, 2014 - by Claude Cox and Mike Kees Nineteen Explorers boarded the County bus at Memorial City Mall on Thursday, June 12th for the day s planned
More informationErosional Features. What processes shaped this landscape?
Have you ever looked at the land around you and wondered what processes shaped what you see? Perhaps you see mountains, valleys, rivers, or canyons. Do you know how long these geologic features have been
More information