Securing a place on the course
|
|
- Gwen Griffith
- 5 years ago
- Views:
Transcription
1 Geological History of Wales: The Evolution of Wales and its Landscape Tutor: John Mason Course code: AE100E Dates: Saturday , and Securing a place on the course To secure a place on the course please ensure that you complete the University enrolment form and returning it signed with the fee. Please download the enrolment form from our website: For current availability of places please phone or or learning@aber.ac.uk Course overview This module builds on 'Geology - An Introduction'. It looks at the geological history of Wales and the landscape produced by hundreds of million years of natural processes such as volcanic eruptions, continental collisions and glacial erosion. The course is largely field-based and is focused on the district between Aberystwyth and Dolgellau. It involves short walks (maximum 4 km). The course is fully accredited by Aberystwyth University giving you the opportunity to study at Higher Education level 2, giving 10 credits which are excellent for professional development. The day-to-day itinerary is as follows: Outline of the Programme Field Trips You will need to be able to walk on steep and rocky ground at times and be reasonably physically fit. The meeting points for the field trips are all detailed below on the maps. Learners will be asked to car share on the field trips. Please note the dates of the field trips may change due to weather conditions. Please be aware that good weather is essential for field trips so dates may be re-arranged if severe conditions are forecast. We will set up an round robin in order to make such arrangements. Therefore these dates are provisional. Annotated maps covering rendezvous points are appended to this document. It is also highly recommended that you have 1:50,000 maps with you too: the Dolgellau (landranger 124) and Aberystwyth (landranger 135) sheets are the ones to have. Day 1: morning lecture at Machynlleth (venue to be confirmed), setting out the framework of the geological evolution of Wales. Beginning with the basics, we then spend the afternoon on the wild and beautiful section of the Cardigan Bay coast at Tonfanau, to the north of Tywyn. Here, participants will learn that most critical of skills - how to identify different rock-types with confidence. Tonfanau is an ideal venue for this because, thanks to the great ice-sheet that flowed down the western seaboard during the peak of the last ice-age, there is an extraordinary diversity
2 of different rock-types present among the boulders. They even include huge blocks of fossiliferous Middle Jurassic limestone, ripped up from the bed of Cardigan Bay and from a time in Earth history that is not represented by rocks on the Welsh mainland. Facilities in Machynlleth and, on the way and way back, at Tywyn. Day 2: Thus primed, we can now look at the rocks where they outcrop and learn to interpret their features. The Welsh landscape is highly variable, even over short distances, the variety being controlled by how different rock-types with differing properties respond to the forces of erosion, such as wind, water, frost, glacial ice and weathering. We go right back to the beginning, in this part of Wales at least, by visiting the Coed y Brenin forest, near Dolgellau. Here, we track the evolution of the early years of the geographical feature that was to dominate Wales from million years ago the marine Welsh Basin, with its variable fill of different types of sediment. We examine rocks deposited under highly energetic conditions and, at the other end of the scale, those deposited in deep water under conditions of marine anoxia, just as much an environmental hazard back then as it is now. Sedimentation in the Welsh Basin was at times disrupted by volcanic activity, a consequence of plate tectonics, and Coed y Brenin features plenty of evidence for magma making its way up through Earth's crust, in the form of sheets of intrusive rock. Many such sheets are horribly altered and mineralised, but we will go and look at two that retain original features, one of which was only rediscovered recently having been lost to science for 90 years and which in the 19 th Century was known as the magnificent Uralite porphyry. The two outcrops record the chemical evolution of a magma chamber beneath Earth's crust, that evolution producing magmas with different properties through time. We will finish off with a spectacular example of how different types of rocks, sedimentary and igneous, affect the type of scenery, at the famous Aerial Bridge. Facilities in Dolgellau, at Coed y Brenin Visitor Centre and in the village of Ganllwyd. Day 3: We take a leap forward in time to 438 million years ago, when rapid climate change and massextinction affected the planet over the boundary between the Ordovician and Silurian Periods. The events are recorded in the sedimentary rocks exposed at Carn Owen, in the hills to the north-east of Aberystwyth, and which also make up much of Mid-Wales. Here, too, we will see the all-tooblatant results of a continental collision, consider how such forces operate and learn how the effects of rock-deformation have affected the Welsh landscape. Following that collision, this part of Wales has remained land ever since. We will discuss how such a conclusion may be arrived at. Visiting a nearby lead-mine, we will then look at evidence for another important on-land phenomenon in landscape-development, deep weathering. There will also be the opportunity to collect samples of lead and copper ores, commodities that were widely sought-after in Wales and which, after everything that came before, have as a consequence left their own distinctive mark on the Welsh landscape. There are no facilities at these locations but in case of dire need, the village of Ponterwyd, a few miles down the road, has the usual range.
3 General information (what to bring) The work will be outdoors but there will be short indoor introductory sessions on the first day. The maximum number on the course will be 12. Clothing Food Students should provide themselves with adequate clothing for fieldwork in the range of weather to be expected in Wales at this time of the year i.e. warm and sunny; and cold and wet. Waterproofs and suitable footwear are essential. Please bring lunches, snacks and drinks with you. Equipment A small A5 field notebook will be provided. Please equip yourself with a pencil (ink isn t usually waterproof) and other writing materials. Increasingly digital cameras are found useful by some students to record details on field trips. A compass and a hand lens will be useful. For further details or questions about the course content please contact Lifelong Learning, Aberystwyth University on or learning@aber.ac.uk
4 MAPS Day One afternoon Tonfanau rendezvous Simply take the Aberdyfi/Tywyn (A493) road, either at Dyfi Bridge near Machynlleth or from the middle roundabout on the A470 Dolgellau by-pass. Either way, Tywyn is on the signpost. If coming from the Aberdyfi direction, continue through Tywyn and turn down L along the lane just after the modern bridge over the Dysinni after the village of Bryncrug. If coming from Dolgellau, head past Fairbourne and Llwyngwril and turn R in Rhoslefain. It's a winding lane so go steady. The parking is on the opposite side of the lane from the small but obvious Tonfanau railway station. No facilities here.
5 Day Two venue rendezvous 1) If coming from the south, travel to Machynlleth and on to Dolgellau. From Dolgellau head north along the A470 (signposted Porthmadog). You will come to a roundabout at Llanelltyd. Continue along the A470, through the village of Ganllwyd, over a substantial river-bridge and commence the long straight climb up out of the valley. Coed Y Brenin Visitor Centre is on the R, up a slanting road (turn-off is well-signposted). If coming from the north, go passt Trawsfynydd and start descending into the valley: the turning is on the L. Head for the car-park ( 3 for 3 hours). 2) Go back down the A470 into Ganllwyd and turn left onto minor road just here:
6 If you miss the turning, you can carry on into the village and turn around by the public loos on the L. In fact it's an easier turn coming out of the village. Follow the lane down and over a stone bridge. Straight ahead for ca. 0.5km until you see a pull-in on the R and NRW sign saying Pont Cae'n-y-Coed. Free parking here. We will move a second time but that will be in convoy, up to the top car-park (again free), at Tyddyn Gwladys. Day Three venue rendezvous The mountain road may be accessed from the A487 in Talybont or the A44 in Ponterwyd. Both are signposted Nant-y-Moch. Follow the road to a point overlooking the N end of the reservoir, where a track strikes off uphill. Ample roadside parking here.
7 We will go in convoy to the mine, which is a mile or two north of Carn Owen. It's up a dirt road just before the mountain road starts to descend to Talybont (OK to drive with care).
School Program Name: Name of Sanctuary: Grade Level: Grades 6 8 Location Options: Time:
School Program Name: Name of Sanctuary: Grade Level: Grades 6 8 Location Options: Time: For more info: Landforms of New England Moose Hill Wildlife Sanctuary At the sanctuary 2 hours or combine with another
More informationRequired Materials Plummer, C., Physical geology. Columbus, OH: McGraw Hill Higher Education
Butler Community College Science, Technology, Engineering, and Math Division Robert Carlson Revised Fall 2017 Implemented Spring 2018 Textbook Update Spring 2018 COURSE OUTLINE Physical Geology Course
More informationMaine Geologic Facts and Localities October, Lobster Lake, Maine. Text by Robert G. Marvinney. Maine Geological Survey
Maine Geologic Facts and Localities October, 1998 Lobster Lake, Maine 45 o 51 7.91 N, 69 o 30 53.88 W Text by Robert G. Marvinney, Department of Agriculture, Conservation & Forestry 1 Map by Introduction
More informationIntroduction to Prospecting. Session Two Geology
Introduction to Prospecting Session Two Geology The Earth Earth is 4.6 billion years old (Ba). Bacteria & algae +3.5 Ba. Microscopic animals ~2 Ba. Animals ~600 million years (Ma) old. Mankind about 100,000
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 information3. [ES 3] 1. [ST8.2] Some processes that shape Earth s surface are slow. Other processes are rapid. Which statement describes a rapid change?
Science 8 SCIENCE QUARTERLY ASSESSMENT 2 3. [ES 3] S 1. [ST8.2] Some processes that shape Earth s surface are slow. Other processes are rapid. Which statement describes a rapid change? A. Glaciers melt
More informationFOSSILS IN YOUR BACKYARD
MOR BACKYARD 12 Activity Overview BIG IDEA OBJECTIVE BACKGROUND Millions of years ago, dinosaurs roamed all over our planet Why is it then that we only find dinosaurs in certain geographical locations?
More informationHigher National Unit specification. General information for centres. Geology and Geomorphology. Unit title: Unit code: F3SL 34
Higher National Unit specification General information for centres Unit title: Geology and Geomorphology Unit code: F3SL 34 Unit purpose: This Unit provides an introduction to geology and geomorphology.
More informationThe Official CA State Science Education Standards for Earth Science K 8
The Official CA State Science Education Standards for Earth Science K 8 Kindergarten The Earth is composed of land, air and water. As a basis for understanding this concept, students know: a. characteristics
More informationField Meeting Report: Coniston, led by Derek Leviston 18 th May 1986
ISSN 1750-855X (Print) ISSN 1750-8568 (Online) Field Meeting Report: Coniston, led by Derek Leviston 18 th May 1986 Les Dolamore 1 DOLAMORE, L. (1987). Field Meeting Report: Carrock Fell, led by Derek
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 informationA Level Geography Cambridge International Content Programme For teaching from September 2016
A Level Geography Cambridge International Content Programme For teaching from September 2016 is located on the Start Bay coast in South Devon and is surrounded by Slapton Ley National Nature Reserve. The
More informationSection 7. Reading the Geologic History of Your Community. What Do You See? Think About It. Investigate. Learning Outcomes
Chapter 3 Minerals, Rocks, and Structures Section 7 Reading the Geologic History of Your Community What Do You See? Learning Outcomes In this section, you will Goals Text Learning Outcomes In this section,
More informationYour web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore
Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore BEDRO CK For the complete encyclopedic entry with media resources,
More informationAnswers: Internal Processes and Structures (Isostasy)
Answers: Internal Processes and Structures (Isostasy) 1. Analyse the adjustment of the crust to changes in loads associated with volcanism, mountain building, erosion, and glaciation by using the concept
More informationGrade 7 Science Revision Sheet for third term final exam
Grade 7 Science Revision Sheet for third term final exam Material for the final exam : 1- Chapter 4 sections 1+2+3+4 [rock cycle + igneous rocks + sedimentary rocks + metamorphic rocks ] pages from the
More informationThis image cannot currently be displayed. Course Catalog. Earth Science Glynlyon, Inc.
This image cannot currently be displayed. Course Catalog Earth Science 2016 Glynlyon, Inc. Table of Contents COURSE OVERVIEW... 1 UNIT 1: DYNAMIC STRUCTURE OF EARTH... 1 UNIT 2: FORCES AND FEATURES OF
More informationEvidence for Continental Drift and The Theory of Plate Tectonics
Evidence for Continental Drift and The Theory of Plate Tectonics Did you know that the coal that is mined in Pennsylvania was actually formed from tropical plant life near the Equator? How did it travel
More informationCoastal Systems and Landscapes 3 days
AS Level Geography WJEC Coastal Systems and Landscapes 3 days This course is for Welsh schools. This in-depth course prepares students for the physical fieldwork focusing on the Coastal option, for Section
More informationName. 4. The diagram below shows a soil profile formed in an area of granite bedrock. Four different soil horizons, A, B, C, and D, are shown.
Name 1. In the cross section of the hill shown below, which rock units are probably most resistant to weathering? 4. The diagram below shows a soil profile formed in an area of granite bedrock. Four different
More informationCurriculum Catalog
2017-2018 Curriculum Catalog 2017 Glynlyon, Inc. Table of Contents EARTH SCIENCE COURSE OVERVIEW...1 UNIT 1: DYNAMIC STRUCTURE OF EARTH... 1 UNIT 2: FORCES AND FEATURES OF EARTH... 1 UNIT 3: FEATURES OF
More informationThe Bedrock Geology of Mount Battie, Camden, Maine
Maine Geologic Facts and Localities July, 2001, Maine 44 13 15.40 N, 69 4 5.10 W Text by Henry N. Berry IV, Department of Agriculture, Conservation & Forestry 1 Photo by Henry N. Berry IV Introduction
More information24. Ocean Basins p
24. Ocean Basins p. 350-372 Background The majority of the planet is covered by ocean- about %. So the majority of the Earth s crust is. This crust is hidden from view beneath the water so it is not as
More informationStation Look at the fossil labeled # 16. Identify each of the following: a. Kingdom b. Phylum c. Class d. Genus
Station 1 1. Look at the fossil labeled # 16. Identify each of the following: a. Kingdom b. Phylum c. Class d. Genus 2. Look at the fossil labeled #7. Identify each of the following: a. Kingdom b. Phylum
More information!!!!! STOP!!!!! What is environmental geology? Earth as a closed system implies nearly everything is cycled, recycled
What is environmental geology?!!!!! STOP!!!!! Geology Study of rocks and minerals that comprise earth s surface and interior and the natural processes that shape the earth s surface and interior over all
More information!!!!! STOP!!!!! What is environmental geology?
!!!!! STOP!!!!! What is environmental geology? Geology Study of rocks and minerals that comprise earth s surface and interior and the natural processes that shape the earth s surface and interior over
More informationA Natural History of our Local Park: Geology and Ecological Succession
Overview This lesson provides an opportunity for students to apply foundational ecological and geological concepts to investigate the natural history of their own local environment. Using field investigation
More informationBeneath our Feet: The 4 Layers of the Earty by Kelly Hashway
Beneath our Feet: The 4 Layers of the Earty by Kelly Hashway The Earth is more than a giant ball made up of dirt, rocks, and minerals. The Earth may look like a giant ball from when looking at it from
More informationEast Penn School District Curriculum and Instruction
East Penn School District Curriculum and Instruction Curriculum for: Geology of National Parks Course(s): Geology of the National Parks Grades: 10-12 Department: Science Length of Period (average minutes):
More informationName Class Date. Study Guide for 7 th Grade Final Exam (Semester One)
Name Class Date Study Guide for 7 th Grade Final Exam (Semester One) 1. What are the steps of the scientific method? Define the problem or question Form a hypothesis (MUST BE TESTABLE) o (identify variables)
More informationEarth Boot Camp. 3.7B: Investigate rapid changes in Earth s surface such as volcanic eruptions, earthquakes and landslides.
Earth Boot Camp 3.7B: Investigate rapid changes in Earth s surface such as volcanic eruptions, earthquakes and landslides. Release Questions 2006 #21 (65%) 1. In which of these ways can volcanoes help
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 informationJurassic Coast Fieldtrip
Field trip leaders: Members of the convener team Dates: Thursday 11 th and Friday 12 th April Jurassic Coast Fieldtrip Logistics: Note that the field trip will begin and end in Piccadilly, London (in front
More informationGEOL 103: Dynamic Earth
gps.gov GEOL 103: Dynamic Earth Syllabus Dr. Antun Husinec Fall 2008 General Description This course is designed to provide you with a basic overview of the science of geology. It is recommended not only
More informationChino Valley Unified School District High School Course Description
CONTACTS 1. School/District Information: School/District: Chino Valley Unified School District Street Address: 5130 Riverside Dr., Chino, CA 91710 Phone: (909) 628-1201 Web Site: chino.k12.ca.us 2. Course
More informationSection 5. Rock Units and Your Community. What Do You See? Think About It. Investigate. Learning Outcomes
Chapter 3 Minerals, Rocks, and Structures Section 5 Rock Units and Your Community What Do You See? Learning Outcomes In this section, you will Recognize that rocks are arranged in Earth s crust as well-defined
More informationQuestion #1: What are some ways that you think the climate may have changed in the area where you live over the past million years?
Reading 5.2 Environmental Change Think about the area where you live. You may see changes in the landscape in that area over a year. Some of those changes are weather related. Others are due to how the
More informationESEU Workshop Learning Outcomes. PRIMARY (England, Northern Ireland and Wales) KS1. Lower KS2. Upper KS2
PRIMARY (England, Northern Ireland and Wales) KS1 Rock circus (for years 1/2) insights into how minerals, rocks, fossils and other things found in the ground can be sorted, classified and identified most
More informationRock Cycle Game and Data Analysis
Rock Cycle Game and Data Analysis Goal: Students use mathematical analysis to deepen their understanding of rock cycle stages and geologic time. Objectives Knowledge: The development of a rock can occur
More informationGeography. Programmes of study for Key Stages 1-3
Geography Programmes of study for Key Stages 1-3 February 2013 Contents Purpose of study 3 Aims 3 Attainment targets 3 Subject content 4 Key Stage 1 4 Key Stage 2 5 Key Stage 3 6 2 Purpose of study A high-quality
More informationDirected Reading page
Skills Worksheet Directed Reading page 185-190 Section: Determining Relative Age 1. How old is Earth estimated to be? 2. Who originated the idea that Earth is billions of years old? 3. On what did the
More informationORIENTEERING. The challenge is to use the map to decide the best route to complete the course in the quickest time. Orienteering Map. Compass.
ORIENTEERING Orienteering is similar to a cross-country race but you navigate using a map instead of following a set course. It is an outdoor sport where competitors navigate their own way, you can run,
More informationPALEOGEOGRAPHY of NYS. Definitions GEOLOGIC PROCESSES. Faulting. Folding 9/6/2012. TOPOGRAPHIC RELIEF MAP of NYS GRADATIONAL TECTONIC
TOPOGRAPHIC RELIEF MAP of NYS PALEOGEOGRAPHY of NYS Prof. Anthony Grande AFG 2012 Definitions GEOLOGIC PROCESSES Geography: study of people living on the surface of the earth. Geology: the scientific study
More informationHigh Impact Forces of Nature Hazards in and Around Rocky Mountain National Park
Stop 1 High Impact Forces of Nature Hazards in and Around Rocky Mountain National Park Trip Leader Vince Matthews, Colorado Geological Survey RMAG on the Rocks July 28, 2007 Welcome to the July RMAG on
More informationGEOLOGY GL1 Foundation Unit
Candidate Name Centre Number Candidate Number 2 General Certificate of Education Advanced Subsidiary/Advanced 451/01 GEOLOGY GL1 Foundation Unit P.M. THURSDAY, 10 January 2008 (1 hour) Examiner Question
More informationName Date Class. Directions: Use the diagram below to answer question Florida Progress Monitoring and Benchmark Assessments
b e n c h m a r k t e s t : e a r t h a n d s p a c e s c i e n c e Multiple Choice 1. Geologists obtain indirect evidence about Earth s interior by A measuring pressure differences at Earth s surface.
More informationOf topic specific knowledge and understanding To encourage progressive development in 'thinking geographically'
[August 2012] Content exemplars 1. Broad description of the content: Single paragraph, written with technical precision Content rigour (avoiding generic statements) Identifying the core of essential knowledge
More informationRocks and the Rock Cycle. Banded Iron Formation
Rocks and the Rock Cycle Banded Iron Formation Rocks Big rocks into pebbles, Pebbles into sand. I really hold a million, million Rocks here in my hand. Florence Parry Heide How do rocks change? How are
More informationExploring geology: The story of the rocks and landscape of the Kettleman Hills
Exploring geology: The story of the rocks and landscape of the Kettleman Hills Table of contents Lesson Plan Details Overview Overarching question Driving questions for students Module description Length
More informationThe University of Jordan. Accreditation & Quality Assurance Center. Course Name: Structural Geology COURSE Syllabus
The University of Jordan Accreditation & Quality Assurance Center COURSE Syllabus Course Name: Structural Geology 0305341 1 Course title Structural Geology 2 Course number 0305341 3 Credit hours (theory,
More informationINTRODUCTION. MRT to magma chamber: field inquiry on plate tectonics and the rock cycle at Little Guilin, Singapore. Field inquiry approach
MRT to magma chamber: field inquiry on plate tectonics and the rock cycle at Little Guilin, Singapore Education and Outreach INTRODUCTION Field inquiry approach This site and the suggested questions and
More informationUNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA
UNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA A map that shows Earth s Topographic Map surface topography, which is Earth s shape and features Contour
More informationSAMPLE PAGE. pulses. The Ice Age By: Sue Peterson
Page 61 Objective sight words (pulses, intermittent, isotopes, chronicle, methane, tectonic plates, volcanism, configurations, land-locked, erratic); concepts (geological evidence and specific terminology
More informationLandscape Development
CHAPTER 22 Landscape Development Chapter Summary Landscapes are described in terms of their topography: elevation, the altitude of the surface of the Earth above sea level; relief, the difference between
More informationGeography Policy 2014
Geography Policy 2014 DEFINITION Geography education should inspire in pupils a curiosity and fascination about the world and its people that will remain with them for the rest of their lives. Teaching
More informationCOURSE OUTLINE Physical Geology
Butler Community College Science, Technology, Engineering, and Math Division Robert Carlson and Kim E. Karr Revised Fall 2011 Implemented Spring 2012 Textbook Update Fall 2015 COURSE OUTLINE Physical Geology
More informationGeohazards in the Himalaya GEOL 3000 (3 Credits / 45 class hours)
Geohazards in the Himalaya GEOL 3000 (3 Credits / 45 class hours) SIT Study Abroad Program: Nepal: Geoscience in the Himalaya PLEASE NOTE: This syllabus represents a recent term. Because courses develop
More informationMap reading made easy
Map reading made easy 1. What is a map? A map is simply a drawing or picture (in 2-D) of a landscape or area of a country (in 3-D). It could be anything from a sketch map for a visitor to find your school
More informationGeology, People, Environment and Sustainable Resources Development of Ladakh
Field Excursions: Geology, People, Environment and Sustainable Resources Development of Ladakh Friday 27 th to Monday 30 th June/ Tuesday 1 st July to Friday 4 th July 2014 Leh and the Ladakh Batholith
More informationPreconference field trip (FT2) - Southern South Island Gold Fields
Preconference field trip (FT2) - Southern South Island Gold Fields OVERVIEW: This field trip to the Otago and Southland goldfields, visits historic sites, and active mines and prospects. The trip will
More informationField Trip to Tempe Butte
Synopsis Field Trip to Tempe Butte So far you have been identifying rocks and mapping their locations without actually going there. Now it is your chance to put it all together and see real rocks out in
More informationGradualism versus Catastrophism Curriculum written by XXXXX
Gradualism versus Catastrophism Curriculum written by XXXXX A curriculum written with the goal of educating 8 th grade science students on the difference between gradual and cataclysmic geological events
More informationChapter 1: Earth as a System
Chapter 1: Earth as a System Science is: Any system of knowledge which tries to observe, identify, understand and describe the nature of the Universe in whole or part. Science explains and predicts the
More informationField Trip Overview Map
CEETEP Field Trip Guide October 11, 2014 Cascadia Subduction Zone CASCADE VOLCANOES COAST RANGE North American Plate get Pu Juan De Fuca Ridge & tte Locked Zone Earthquake me MID-OCEAN RIDGE lla Pacific
More informationYou Might Also Like. Thanks. Connect
Thanks 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 at my blog
More informationThe Geology of the Marginal Way, Ogunquit, Maine
Maine Geologic Facts and Localities February, 2002 The Geology of the Marginal Way, Ogunquit, Maine 43 14 23.88 N, 70 35 18.36 W Text by Arthur M. Hussey II, Bowdoin College and Robert G. Marvinney,, Department
More informationWhat landforms make up Australia?!
What landforms make up Australia? The tectonic forces of folding, faulting and volcanic activity have created many of Australia's major landforms. Other forces that work on the surface of Australia, and
More informationMap reading made easy
Map reading made easy 1 1. What is a map? A map is simply a drawing or picture (in 2-D) of a landscape or area of a country (in 3-D). It could be anything from a sketch map for a visitor to find your school
More informationfor EDC Earth Science EDC Earth Science features the following design components:
LAB- AIDS Correlations to Georgia Science Standards of Excellence 2016 for EDC Earth Science ABOUT EDC EARTH SCIENCE EDC Earth Science is a full year, activity- driven high school earth science course
More informationPSc 201 Chapter 3 Homework. Critical Thinking Questions
PSc 201 Chapter 3 Homework Critical Thinking Questions 1. (adapted from text) Seawater is denser than fresh water. A ship moving from the Atlantic Ocean into the Great Lakes goes from seawater to fresh
More informationNAMAQUA METAMORPHIC PROVINCE FIELD TRIP
- 2016 NAMAQUA METAMORPHIC PROVINCE FIELD TRIP Theme: GEOLOGY AND ORIGIN OF A VERY LARGE HOT OROGEN - THE HIGH-T-LOW-P NAMAQUA METAMORPHIC PROVINCE 21-27 August 2016 Pre-conference field trip Geology to
More informationGeology 109L Lab 3: Modern Sedimentary Environments --Field Trip to Bodega Bay--
Geology 109L Lab 3: Modern Sedimentary Environments --Field Trip to Bodega Bay-- Goal: The purpose of this lab is to recognize characteristics of modern sedimentary environments, which will aid you in
More informationCoastal Landscapes Case Study 3 days
GCSE Geography OCR A Coastal Landscapes Case Study 3 days In-depth study of a coastal landscape providing a detailed case study, to ensure students are prepared for the Paper 1 exam: Living in the UK Today.
More informationWhat is a map? Understanding your map needs
What is a map? A map is simply a drawing or picture of a landscape or location. Maps usually show the landscape as it would be seen from above, looking directly down. As well as showing the landscape of
More informationSocial Studies. Chapter 2 Canada s Physical Landscape
Social Studies Chapter 2 Canada s Physical Landscape Introduction Canada s geography its landforms and climate - has a great impact on Canadians sense of identity. Planet Earth The earth is divided into
More informationGEOLOGY (GEOL) Geology (GEOL) 1. GEOL 118 Societal Issues in Earth Science (4 crs)
Geology (GEOL) 1 GEOLOGY (GEOL) GEOL 102 Oceanography (3 crs) Survey of the world oceans with emphasis on geologic processes. Also includes chemical, physical, and biological aspects of the sea. Investigates
More informationCoastal Landscapes Case Study 3 days
GCSE Geography OCR B Coastal Landscapes Case Study 3 days In-depth study of a coastal landscape providing a detailed case study, to ensure students are prepared for Paper 1: Our Natural World. Complete
More informationSection 11.1 pp Where Mountains Form
Section 11.1 pp. 236 237 Where Mountains Form Chapter 11 Set a Purpose: TE, p. 236 Reading Study Guide, p. 36 Discussion: TE, p. 236 Differentiating ion Reading Support: TE, p. 236 Visual Teaching Interpret
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 informationBenchmark #: State Language: Student Friendly Language: The student models earth s cycles, constructive and
Science, Grade: 7 Mastery Check Benchmark #: 7.4.1.2 4 State Language: Student Friendly Language: The student models earth s cycles, constructive and I will be able to describe weathering, erosion, and
More informationWe will provide: hammers (one per group), hard hats, shovels, paper bags or boxes for pebble collections, map boards, and compasses, measuring tapes.
Geology 110 Spring 1999 Northfield Topography and Field Trip to Little Chicago This lab has two parts. After the spot test on the geologic time scale, we will spend the next few hours at a gravel pit near
More informationHiking the Bold Coast, Cutler, Maine
Maine Geologic Facts and Localities June, 2010 Hiking the Bold Coast, Cutler, Maine 44 o 39 36.34 N, 67 o 12 46.99 W Text by Robert A. Johnston, Department of Agriculture, Conservation & Forestry 1 Map
More informationIowa s Tectonic Future * Created by Kyle N. Hoffman, Geology, Linn-Mar High School, Marion Iowa. 2009
Iowa s Tectonic Future * Created by Kyle N. Hoffman, Geology, Linn-Mar High School, Marion Iowa. 2009 Teachers Notes Objectives: - Students will demonstrate knowledge of the rock cycle - Students will
More informationA Living Planet. Chapter PHYSICAL GEOGRAPHY. What you will learn in this chapter. Summary of the chapter
QUIT Main Ideas What you will learn in this chapter Summary Summary of the chapter Test your geographic knowledge by playing the. Main Ideas Section 1: The Earth Inside and Out The earth is the only habitable
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 informationCrissy Field Rocks! Crissy Field Center Community Group Programs. A Partnership of: National Park Service. Golden Gate National Parks Conservancy
Crissy Field Rocks! Crissy Field Center Community Group Programs A Partnership of: National Park Service Golden Gate National Parks Conservancy Presidio Trust 1 Group Leader Pre-Visit Packet Crissy Field
More informationPHYSICAL GEOLOGY SYLLABUS GLY 1010 Physical Geology Fall
PHYSICAL GEOLOGY SYLLABUS GLY 1010 Physical Geology Fall - 2011 Instructor s Name: Marianne O Neal Caldwell Telephone Number: (813) 253-7251 Email Address: Please use the email in our online classroom.
More informationTuesday, September 05, 2017 Planet Earth
Tuesday, September 05, 2017 Planet Earth Objective: Describe the solar system and Earth s location in it. Identify Earth s shape. Discuss Earth s structure. List Earth s landforms Do Now: What is a compass
More information1- Water on Earth 2- Oceans and seas / continental waters 3- Uses, risks and problems of water
Contents: I- Relief 1- Structure of the Earth and relief formation 2- Shaping of relief 3- Types of relief II- Water 1- Water on Earth 2- Oceans and seas / continental waters 3- Uses, risks and problems
More informationErosion and Deposition along Rivers and Seashores - Part 1: Modeling in the Classroom
Erosion and Deposition along Rivers and Seashores - Part 1: Modeling in the Classroom Lesson Focus: Erosion and Deposition Learning Objectives: Students will learn to recognize landforms found on Earth.
More informationMaterials needed: ISNs (students & teacher), document camera, self-reflection pages, corrected tests
Science April 6-10 L.HE.05.11 Explain that the traits of an individual are influenced by both the environment and the genetics of the individual. L.HE.05.12 Distinguish between inherited and acquired traits.
More informationChapter 2: Physical Geography
Chapter 2: Physical Geography Pg. 39-68 Learning Goals for Chp2: q q q q q Explain how the Earth moves in space and why seasons change. Outline the factors that influence climate and recognize different
More informationGEOG 1010A. Come to the PASS workshop with your mock exam complete. During the workshop you can work with other students to review your work.
It is most beneficial to you to write this mock midterm UNDER EXAM CONDITIONS. This means: Complete the midterm in 1.5 hours. Work on your own. Keep your notes and textbook closed. Attempt every question.
More informationThe performance expectation above was developed using the following elements from the NRC document A Framework for K-12 Science Education:
MS-ESS2-1 Earth's Systems Students who demonstrate understanding can: MS-ESS2-1. Develop a model to describe the cycling of Earth's materials and the flow of energy that drives this process. [Clarification
More informationWHAT IS THE EARTH MADE OF? LITHOSPHERE AND HYDROSPHERE
UNIT 8 WHAT IS THE EARTH MADE OF? LITHOSPHERE AND HYDROSPHERE TABLE OF CONTENTS 1 THE STRUCTURE OF THE EARTH... 2 2 THE FORMATION OF THE RELIEF: INTERNAL AND EXTERNAL FORCES.... 2 2.1 Internal forces:
More informationExploring Geography. Chapter 1
Exploring Geography Chapter 1 The Study of Geography Geography is the study of where people, places, and things are located and how they relate to each other. Greek meaning writing about or describing
More informationLandscape Systems: Glaciation 3 days
AS Level Geography Edexcel Landscape Systems: Glaciation 3 days Deliver two days of fieldwork within an inspiring physical environment covering all the recommended themes in depth. Prepare AS level students
More information4 th Grade PSI. Slide 1 / 107 Slide 2 / 107. Slide 3 / 107. Slide 4 / 107. Slide 5 / 107. Slide 6 / 107. The History of Planet Earth
Slide 1 / 107 Slide 2 / 107 4 th Grade PSI The History of Planet Earth 2015-11-10 www.njctl.org Slide 3 / 107 Slide 4 / 107 The History of Planet Earth The Structure of Earth Rock Layers Fossils and Relative
More informationGLY 155 Introduction to Physical Geology, W. Altermann. Press & Siever, compressive forces. Compressive forces cause folding and faulting.
Press & Siever, 1995 compressive forces Compressive forces cause folding and faulting. faults 1 Uplift is followed by erosion, which creates new horizontal surface. lava flows Volcanic eruptions cover
More informationGeography Curriculum. Key Stage 1
Geography Curriculum Key Stage 1 Year 1 In the first term, students explore a variety of maps of the local environment, including the Academy grounds. They use a paper location to plan a route. They also
More information