Papaver gorodkovii Volcanic Scree Plant Association Arctic Poppy Volcanic Scree Plant Association Western Alaska

Size: px
Start display at page:

Download "Papaver gorodkovii Volcanic Scree Plant Association Arctic Poppy Volcanic Scree Plant Association Western Alaska"

Transcription

1 Papaver gorodkovii Volcanic Scree Plant Association Arctic Poppy Volcanic Scree Plant Association Western Alaska Conservation Status Rank: S3 (vulnerable) Introduction The Papaver gorodkovii (Arctic poppy) Volcanic Scree plant association occurs on nearly barren volcanic scree slopes supporting a sparse vegetation cover dominated by the rare plant Papaver gorodkovii (Figure 1). As a species, Papaver gorodkovii is endemic to western and northern Alaska and eastern Siberia where it typically occurs on sparsely vegetated coastal back dunes, river gravel bars, and limestone talus (Nawrocki et al. 2013). Its occurrence on volcanic scree slopes has only been observed on Nunivak and St. Lawrence islands. Figure 1. Papaver gorodkovii growing on volcanic scree, Nunivak Island, Bering Sea, Alaska. Distribution This association is documented from Nunivak and St. Lawrence islands only, but is suspected to occur on volcanic scree in western mainland Alaska. Papaver gorodkovii is a Beringian species endemic to coastal areas of western and northern Alaska, Wrangel Island in northeast Siberia, and has been reported but not confirmed from the Canadian Arctic Archipelago (Nawrocki et al. 2013). The distribution of this association was developed from the intersection of herbarium records (CPNWH 2016) of Papaver gorodkovii with the young volcanic scree and shallow intrusive rocks group of the Geologic Map of Alaska (Wilson et al. 2015) (Figure 2). 1

2 Figure 2. Distribution of the Papaver gorodkovii Volcanic Scree Plant Association on the Bering Sea Islands, Alaska. Note that point occurrences in this map are buffered for greater visibility. Climate In western Alaska, the climate is maritime near the coast to subarctic continental away from the coast and at the higher elevations (NRCS, 2004). In the northern part of the region, the winter climate becomes more continental as the icepack forms in the Bering Sea. Summers are short and warm and cloudy along the coast, and winters are long and cold. The annual precipitation ranges from about 33 to 203 cm with the lowest precipitation in lowland areas and the highest at the higher elevations of the Ahklun and Alaska Peninsula. The average annual temperature ranges from -4 to 2 o C Frost may occur in any month, strong winds are common, and snow covers the ground for approximately 7 to 9 months each year. Environmental Characteristics This plant association occurs from 100 m to 500 m on moderate to steep (10 to 20 degree) volcanic scree slopes of the Nunivak and St. Lawrence Islands. Soils are mesic to dry and comprised of gravel or small volcanic rocks (lapilli) overlying fine-grained mineral soil. Biological crusts often develop on finer-grained surface soils. 2

3 The central part of St. Lawrence Island is dominated by the Kookooligit Mountains, a large Quaternary shield volcano with abundant, thin pahoehoe lava flows, smaller alkali basalt lava flows, cinder cones, and maars (Wood and Kienle 1990, Hoare et al. 1968). Volcanic deposits are underlain by Cretaceous sedimentary rock. On both Nunivak and St. Lawrence islands, this plant association occurs on eroding basalt bedrock slopes with fine, loose lapilli. In areas of basalt bedrock, Papaver gorodkovii occurs in patches of unstable gravel (Figure 3, Figure 4, Figure 5). Figure 3. The rare plant Papaver gorodkovii (G3 S2S3) growing on weathered basalt, Nunivak Island, Alaska. Vegetation and Succession Papaver gorodkovii dominates this sparselyvegetated type, minor associates include Cassiope tetragona ssp. tetragona, Chamerion latifolium, Chrysosplenium wrightii, Corydalis arctica, Poa arctica, Poa pratensis var. colpodea, Ranunculus nivalis, Racomitrium spp., Salix ovalifolia var. glacialis, and Thamnolia vermicularis. Papaver gorodkovii is a perennial forb that is presumably insect-pollinated, and likely to be long-lived based on extensive caudexes with persistent leaf bases. No vegetation successional studies have been conducted. Based on observations, the Papaver gorodkovii plant association is an early seral colonizer of active volcanic scree surfaces (Bos 1967). Primary succession on volcanic surfaces may be limited by direct climatic effects rather than by nutrients (Wood & del Moral 1993). Conservation Status Rarity: The Papaver gorodkovii volcanic scree plant association is known from only five locations on volcanic cones of Nunivak Island (Figure 4) and St. Lawrence Island. Further survey is needed to determine if it occurs elsewhere in Western Alaska. A few herbarium records of Papaver gorodkovii occur in the Northern Alaska ecoregion including records from Point Barrow, Prudhoe Bay, Canning River vicinty, Point Hope, and Cape Lisburne. Threats: While no nonnative plants are known from regions around this plant association, establishment of invasive species could pose a threat. Remote areas of other islands in Alaska (e.g. Camp Island on Kodiak) have been invaded by invasive species, such as orange hawkweed (AKEPIC 2016). Additionally, the rapidly changing climate poses a potential threat to the persistence of the species composing this plant association, tracking suitable climate envelopes for insular species is particularly problematic (Carlson and Cortes-Burns 2013). Trend: The extent and condition of this association is not expected to change in the short- or long-term. 3

4 Figure 4. View from an alkali basalt cone on Nunivak Island, Alaska. Figure 5. The Papaver gorodkovii Plant Association on weathered basalt, St. Lawrence Island. Species of Conservation Concern Papaver gorodkovii is the only plant species of concern so far identified in this plant association. This plant is considered globally vulnerable (ranked G3, S2S3) as there are only 20 known locations in eastern Russia 4

5 and northern Alaska. It is also considered a sensitive species requiring special management consideration to promote its conservation by the BLM in Alaska. Please visit the Alaska Center for Conservation Science website for a full species description (ACCS 2016). The bird species listed below is designated vulnerable within Alaska (S1-S3) and is suspected to occur in this plant association (Table 1). Please visit the Alaska Center for Conservation Science website for species descriptions (ACCS 2016). Table 1. Bird species of conservation concern within the Papaver gorodkovii Plant Association. Common Name Scientific Name Global Rank State Rank Habitat Description Birds McKay s Bunting Plectrophenax hyperboreus GU S3 May use coastal habitat in the Bering Sea including Nunivak Island during migration. This species is only known to breed on St. Matthews and Hall islands in rocky areas and beaches but could also use rocky areas and crevices within this plant association on Nunivak Island. Classification Concept Source This publication represents the first description of the Papaver gorodkovii volcanic scree plant association. Literature Cited ACCS (Alaska Center for Conservation Science) Rare Plant Data Portal. April 28, ACCS (Alaska Center for Conservation Science) BIOTICS Animal Data Portal. April 28, AKEPIC (2016). Alaska Exotic Plant Information Clearinghouse database ( Alaska Center for Conservation Science, University of Alaska, Anchorage. Accessed (April, 30, 2016). Bos, G. N Range types and their utilization by muskox on Nunivak Island, Alaska: A reconnaissance study. Master s Thesis, University of Alaska. 113 pp. Carlson, M. L., and H. Cortes-Burns Rare Vascular Plant Distributions in Alaska: Evaluating Patterns of Habitat Suitability in the Face of Climate Change. In: Gibble, W., J. Combs, and S. Reichard. (eds.) Conserving Plant Biodiversity in a Changing World: a View from Northwestern North America. University of Washington Botanic Gardens. Conference Proceedings, 106 pp. Consortium of Pacific Northwest Herbaria (CPNWH). Burke Museum, University of Washington. Herbarium specimen data provided by: University of Alaska, Fairbanks Museum of the North, University of Alaska Anchorage Herbarium. Herbarium specimen data accessed February 2016 from: Hoare, J. M., W. H. Condon, A. Cox, and G. B. Dalrymple Geology, paleomagnetism, and potassium-argon ages of basalts from Nunivak Island, Alaska. Pages in R. R. Coats, R. L. Hay, and C. A. Anderson, eds. Studies in volcanology, Geological Society of America Memoir MWR National Resource Conservation Service (NRCS) Land resource regions and major land resource areas of Alaska. United States Department of Agriculture Natural Resources Conservation Service. Palmer, Alaska. Nawrocki, T., J. Fulkerson, and M. Carlson Alaska Rare Plant Field Guide. Alaska Natural Heritage Program, University of Alaska Anchorage. 352 pp. 5

6 Wilson, F.H., C.P. Hults, C.G. Mull, and S.M. Karl Geologic map of Alaska: U.S. Geological Survey Scientific Investigations Map 3340, pamphlet 196 p., 2 sheets, scale 1:1,584,000, Wood, C. A., and J. Kienle, eds Volcanoes of North America: United States and Canada: New York, Cambridge University Press, 354 pp. Wood, D. M. and Roger del Moral Primary succession at the volcano Mt. St. Helens. Journal of Vegetation Ecology. Volume 4:2 pp

Luzula confusa-poa arctica Plant Association Northern Woodrush-Arctic Bluegrass Plant Association Northern Alaska

Luzula confusa-poa arctica Plant Association Northern Woodrush-Arctic Bluegrass Plant Association Northern Alaska Luzula confusa-poa arctica Plant Association Northern Woodrush-Arctic Bluegrass Plant Association Northern Alaska Conservation Status Rank: S4 (apparently secure) Introduction The Luzula confusa-poa arctica

More information

Chapter 6, Part Colonizers arriving in North America found extremely landscapes. It looked different to region showing great.

Chapter 6, Part Colonizers arriving in North America found extremely landscapes. It looked different to region showing great. Social Studies 9 Unit 1 Worksheet Chapter 6, Part 1. 1. Colonizers arriving in North America found extremely landscapes. It looked different to region showing great. 2. The Earth is years old and is composed

More information

Social Studies. Chapter 2 Canada s Physical Landscape

Social 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 information

discussion of North America s physical features, including its landforms and bodies of

discussion of North America s physical features, including its landforms and bodies of Chapter 7 Natural Environments of North America Chapter 7 focuses on the natural environments of North America. The chapter opens with a discussion of North America s physical features, including its landforms

More information

EQ: Discuss main geographic landforms of the U.S. & Canada and examine varied landforms in relation to their lifestyles.

EQ: Discuss main geographic landforms of the U.S. & Canada and examine varied landforms in relation to their lifestyles. EQ: Discuss main geographic landforms of the U.S. & Canada and examine varied landforms in relation to their lifestyles. Places & Terms for Discussion Appalachian Mountains Great Plains Canadian Shield

More information

Tropical Moist Rainforest

Tropical Moist Rainforest Tropical or Lowlatitude Climates: Controlled by equatorial tropical air masses Tropical Moist Rainforest Rainfall is heavy in all months - more than 250 cm. (100 in.). Common temperatures of 27 C (80 F)

More information

The United States & Canada. A Regional Study of Anglo America

The United States & Canada. A Regional Study of Anglo America A Regional Study of Anglo America Landform Regions of the United States & Canada world leaders in agricultural and industrial production because of... VAST LANDS stretch from the Atlantic Ocean on the

More information

Alaska Statewide Climate Summary February 2019

Alaska Statewide Climate Summary February 2019 Alaska Statewide Climate Summary February 2019 The following report provides an overview of the February 2019 weather. The report is based on preliminary data from selected weather stations throughout

More information

Grade 9 Social Studies Canadian Identity. Chapter 2 Review Canada s Physical Landscape

Grade 9 Social Studies Canadian Identity. Chapter 2 Review Canada s Physical Landscape Grade 9 Social Studies Canadian Identity Chapter 2 Review Canada s Physical Landscape Name: Unit 1: Empowerment Terms (notes or textbook) 1. Core 2. Crust 3. Mantle 4. Magma 5. Continental drift 6. Plate

More information

Ecoregions Glossary. 7.8B: Changes To Texas Land Earth and Space

Ecoregions 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 information

Fig Major air masses of the world

Fig Major air masses of the world Fig. 9.3 Major air masses of the world CLASSIFICATION FOUR BASIC CATEGORIES OF AIR MASSES: POLAR - P ARCTIC - A TROPICAL - T EQUATORIAL - E TWO DESIGNATIONS OF SURFACE IN SOURCE REGION MARITIME - m. CONTINENTAL

More information

Papaver Alboroseum Portage Poppy. Katie Shields Hort 5051 May 4, 2005

Papaver Alboroseum Portage Poppy. Katie Shields Hort 5051 May 4, 2005 Papaver Alboroseum Portage Poppy Katie Shields Hort 5051 May 4, 2005 Taxonomy Scientific Name: Papaver alboroseum Synonyms: None Common Names: Portage Poppy, Pale Poppy, Pink Poppy Family: Papaveraceae

More information

Field Survey for Laramie Columbine. (Aquilegia laramiensis) In the Rawlins Field Office

Field Survey for Laramie Columbine. (Aquilegia laramiensis) In the Rawlins Field Office Field Survey for Laramie Columbine (Aquilegia laramiensis) In the Rawlins Field Office prepared for the Wyoming Natural Diversity Database, University of Wyoming, and the Bureau of Land Management, Rawlins

More information

AIR MASSES. Large bodies of air. SOURCE REGIONS areas where air masses originate

AIR MASSES. Large bodies of air. SOURCE REGIONS areas where air masses originate Large bodies of air AIR MASSES SOURCE REGIONS areas where air masses originate Uniform in composition Light surface winds Dominated by high surface pressure The longer the air mass remains over a region,

More information

The elevations on the interior plateau generally vary between 300 and 650 meters with

The elevations on the interior plateau generally vary between 300 and 650 meters with 11 2. HYDROLOGICAL SETTING 2.1 Physical Features and Relief Labrador is bounded in the east by the Labrador Sea (Atlantic Ocean), in the west by the watershed divide, and in the south, for the most part,

More information

UNIT SEVEN: Earth s Water. Chapter 21 Water and Solutions. Chapter 22 Water Systems. Chapter 23 How Water Shapes the Land

UNIT SEVEN: Earth s Water. Chapter 21 Water and Solutions. Chapter 22 Water Systems. Chapter 23 How Water Shapes the Land UNIT SEVEN: Earth s Water Chapter 21 Water and Solutions Chapter 22 Water Systems Chapter 23 How Water Shapes the Land Chapter Twenty-Three: How Water Shapes the Land 23.1 Weathering and Erosion 23.2

More information

Beringian Alpine Limestone Dryas Biophysical Setting Northern and Western Alaska

Beringian Alpine Limestone Dryas Biophysical Setting Northern and Western Alaska Beringian Alpine Limestone Dryas Biophysical Setting Northern and Western Alaska Conservation Status Rank: S4 (apparently secure) Introduction The Beringian Alpine Limestone Dryas Biophysical Setting occurs

More information

Landforms in Canada. Canada is made up of three dis;nct types of landforms: Canadian Shield Highlands Lowlands

Landforms in Canada. Canada is made up of three dis;nct types of landforms: Canadian Shield Highlands Lowlands Canada s Landforms What is a Landform? A landform is any physical feature of the Earth s surface having a characteris;c, recognizable shape, produced by natural causes. Landforms include major features

More information

The Marine Environment

The Marine Environment The Marine Environment SECTION 16.1 Shoreline Features In your textbook, read about erosional landforms, beaches, estuaries, longshore currents, and rip currents. For each statement below, write or. 1.

More information

Markville. CGC 1DL/PL Geography. Geography of Canada. Natural Environment Unit Test

Markville. CGC 1DL/PL Geography. Geography of Canada. Natural Environment Unit Test Markville CGC 1DL/PL Geography Geography of Canada Natural Environment Unit Test Name: Thinking /10 Knowledge /10 Application /10 Communication /10 Part A: Blanks (1 mark each) Thinking Choose the correct

More information

THE CHANGING SURFACE OF THE EARTH

THE 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 information

Unit 2. United States Physical Geography

Unit 2. United States Physical Geography Unit 2 United States Physical Geography Physical Geography U.S. extends from the Atlantic to Pacific U.S. is the 3rd largest country U.S. has fertile soils, vast forests, and variety of minerals All major

More information

Through their research, geographers gather a great deal of data about Canada.

Through their research, geographers gather a great deal of data about Canada. Ecozones What is an Ecozone? Through their research, geographers gather a great deal of data about Canada. To make sense of this information, they often organize and group areas with similar features.

More information

CANADA S LANDFORM REGIONS

CANADA S LANDFORM REGIONS CANADA S LANDFORM REGIONS Canada s Regions Canada is divided into Eight major regions. A Region is an area that is defined on the basis of the presence or absence of certain characteristics: Age of rock

More information

Northwest Outlook October 2016

Northwest Outlook October 2016 Northwest Outlook October 2016 Rainfall Opportunities and Challenges Rainfall over the month of September presented some challenges for the fall harvest while other producers benefitted. Figure 1a shows

More information

What is the largest country in the world? Russia

What is the largest country in the world? Russia What is the largest country in the world? #1 Russia CSCOPE 2007 2 Russia Dimensions #2-3 Spans 11 Time Zones From East to West: Gulf of Finland to Alaska From North to South: Above the Arctic Circle to

More information

GLOBAL CLIMATES FOCUS

GLOBAL CLIMATES FOCUS which you will learn more about in Chapter 6. Refer to the climate map and chart on pages 28-29 as you read the rest of this chapter. FOCUS GLOBAL CLIMATES What are the major influences on climate? Where

More information

6. What has been the most effective erosive agent in the climate system? a. Water b. Ice c. Wind

6. What has been the most effective erosive agent in the climate system? a. Water b. Ice c. Wind Multiple Choice. 1. Heinrich Events a. Show increased abundance of warm-water species of planktic foraminifera b. Show greater intensity since the last deglaciation c. Show increased accumulation of ice-rafted

More information

National Wildland Significant Fire Potential Outlook

National Wildland Significant Fire Potential Outlook National Wildland Significant Fire Potential Outlook National Interagency Fire Center Predictive Services Issued: April 1, 2008 Next Issue: May 1, 2008 Wildland Fire Outlook April 2008 through July 2008

More information

How does the physical environment influence communities and ecosystems? Hoodoos in Cappadocia, Turkey

How does the physical environment influence communities and ecosystems? Hoodoos in Cappadocia, Turkey Biomes of the World How does the physical environment influence communities and ecosystems? Hoodoos in Cappadocia, Turkey ecosystems are shaped by: abiotic factors climate/weather space Rainfall Soil air

More information

Objectives: Define Relative Age, Absolute Age

Objectives: Define Relative Age, Absolute Age S6E5. Students will investigate the scientific view of how the earth s surface is formed. c. Classify rocks by their process of formation. g. Describe how fossils show evidence of the changing surface

More information

Weathering, Erosion, Deposition, and Landscape Development

Weathering, Erosion, Deposition, and Landscape Development Weathering, Erosion, Deposition, and Landscape Development I. Weathering - the breakdown of rocks into smaller particles, also called sediments, by natural processes. Weathering is further divided into

More information

Mediterranean Climates (Csa, Csb)

Mediterranean Climates (Csa, Csb) Climatic Zones & Types Part II I've lived in good climate, and it bores the hell out of me. I like weather rather than climate. 1 John Steinbeck Mediterranean Climates (Csa, Csb) Main locations Western

More information

Figure 1 The map shows the top view of a meandering stream as it enters a lake. At which points along the stream are erosion and deposition dominant?

Figure 1 The map shows the top view of a meandering stream as it enters a lake. At which points along the stream are erosion and deposition dominant? 1. In which type of climate does chemical weathering usually occur most rapidly? 1. hot and dry 3. cold and dry 2. hot and wet 4. cold and wet 2. Figure 1 The map shows the top view of a meandering stream

More information

Continental Landscapes

Continental Landscapes Continental Landscapes Landscape influenced by tectonics, climate & differential weathering Most landforms developed within the last 2 million years System moves toward an equilibrium Continental Landscapes

More information

Chapter 3 Section 3 World Climate Regions In-Depth Resources: Unit 1

Chapter 3 Section 3 World Climate Regions In-Depth Resources: Unit 1 Guided Reading A. Determining Cause and Effect Use the organizer below to show the two most important causes of climate. 1. 2. Climate B. Making Comparisons Use the chart below to compare the different

More information

3/24/2016. Geology 12 Mr. M. Gauthier 24 March 2016

3/24/2016. Geology 12 Mr. M. Gauthier 24 March 2016 Geology 12 Mr. M. Gauthier 24 March 2016 Introduction: Mt. St. Helens Before 1980 Mt. St Helens, in Southern Washington State, had not erupted since 1857 On March 27,1980 minor ashand eruptions were due

More information

(version 3) I. HumAN -Environment Interaction

(version 3) I. HumAN -Environment Interaction (version 3) I. HumAN -Environment Interaction A. Landforms 1. Earth s topography is made up of many different types of landforms. 2. While the planet is covered primarily with water, the four major types

More information

Wednesday, November 15, 2017

Wednesday, November 15, 2017 Wednesday, November 15, 2017 Northern Europe: Physical Geography Objective: Locate and describe the various traditional regions of Western Europe. Outline how the physical geography varies from region

More information

March 1, 2003 Western Snowpack Conditions and Water Supply Forecasts

March 1, 2003 Western Snowpack Conditions and Water Supply Forecasts Natural Resources Conservation Service National Water and Climate Center 101 SW Main Street, Suite 1600 Portland, OR 97204-3224 Date: March 17, 2003 Subject: March 1, 2003 Western Snowpack Conditions and

More information

Sediment and Sedimentary rock

Sediment and Sedimentary rock Sediment and Sedimentary rock Sediment: An accumulation of loose mineral grains, such as boulders, pebbles, sand, silt or mud, which are not cemented together. Mechanical and chemical weathering produces

More information

The Marine Environment

The Marine Environment The Marine Environment SECTION 16.1 Shoreline Features In your textbook, read about erosional landforms, beaches, estuaries, longshore currents, and rip currents. For each statement below, write true or

More information

LANDFORM REGIONS IN CANADA. Classroom Notes and Descriptions

LANDFORM REGIONS IN CANADA. Classroom Notes and Descriptions LANDFORM REGIONS IN CANADA Classroom Notes and Descriptions Landform Regions in Canada There are eight distinct landforms in Canada: Western Cordillera Region Interior Plains Canadian Shield Hudson Bay

More information

Grade 9 Geography Chapter 11 - Climate Connections

Grade 9 Geography Chapter 11 - Climate Connections Grade 9 Geography Chapter 11 - Climate Connections 1. Define: Weather. 2. In what way has weather affected your activities in the last two weeks? 3. Define: Climate. 4. Canada s climate is a function of

More information

Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa

Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa Weather Patterns and Severe Weather Foundations, 6e - Chapter 14 Stan Hatfield Southwestern Illinois College Air masses Characteristics Large body

More information

Physical Geology, 15/e

Physical Geology, 15/e Lecture Outlines Physical Geology, 15/e Plummer, Carlson & Hammersley Weathering and Soil Physical Geology 15/e, Chapter 5 Weathering, Erosion and Transportation Rocks exposed at Earth s surface are constantly

More information

Our climate system is based on the location of hot and cold air mass regions and the atmospheric circulation created by trade winds and westerlies.

Our climate system is based on the location of hot and cold air mass regions and the atmospheric circulation created by trade winds and westerlies. CLIMATE REGIONS Have you ever wondered why one area of the world is a desert, another a grassland, and another a rainforest? Or have you wondered why are there different types of forests and deserts with

More information

TAKE HOME EXAM 8R - Geology

TAKE HOME EXAM 8R - Geology Name Period Date TAKE HOME EXAM 8R - Geology PART 1 - Multiple Choice 1. A volcanic cone made up of alternating layers of lava and rock particles is a cone. a. cinder b. lava c. shield d. composite 2.

More information

Social Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE

Social Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE Social Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE The Structure of the Earth To understand the forces that create Canada's physical landscape we must understand the structure

More information

Internet Interactive Rock Cycle

Internet 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 information

01/12/2016. Introduction. Planet Earth. Plate Tectonics. Social Studies

01/12/2016. Introduction. Planet Earth. Plate Tectonics. Social Studies Introduction Social Studies Chapter 2 Canada s Physical Landscape Canada s geography its landforms and climate - has a great impact on Canadians sense of identity. Planet Earth The earth is divided into

More information

Colorado CoCoRaHS. Colorado CoCoRaHS. Because Every Drop Counts! November 2014 Volume 2, Issue 11

Colorado CoCoRaHS. Colorado CoCoRaHS. Because Every Drop Counts! November 2014 Volume 2, Issue 11 U.S. PRECIPITATION (% OF AVERAGE) LOOKING BACK AT OCTOBER 2014 October was a fairly dry month for much of the nation with the exception of the Pacific Northwest, portions of New England and the Tennessee

More information

World Geography Chapter 3

World Geography Chapter 3 World Geography Chapter 3 Section 1 A. Introduction a. Weather b. Climate c. Both weather and climate are influenced by i. direct sunlight. ii. iii. iv. the features of the earth s surface. B. The Greenhouse

More information

Weather is the day-to-day condition of Earth s atmosphere.

Weather is the day-to-day condition of Earth s atmosphere. 4.1 Climate Weather and Climate Weather is the day-to-day condition of Earth s atmosphere. Climate refers to average conditions over long periods and is defined by year-after-year patterns of temperature

More information

Study 11.9 Invasive Plant Study

Study 11.9 Invasive Plant Study Initial Study Report Update Meeting Study 11.9 Invasive Plant Study March 29, 2016 Prepared by ABR, Inc. Environmental Research & Services 10/21/2014 1 Study 11.9 Status ISR documents (ISR Part D Overview):

More information

How does the greenhouse effect maintain the biosphere s temperature range? What are Earth s three main climate zones?

How does the greenhouse effect maintain the biosphere s temperature range? What are Earth s three main climate zones? Section 4 1 The Role of Climate (pages 87 89) Key Concepts How does the greenhouse effect maintain the biosphere s temperature range? What are Earth s three main climate zones? What Is Climate? (page 87)

More information

TOPOGRAPHIC RELIEF MAP of NYS. LANDFORMS of NYS. Landforms. Creation of NYS Landforms 9/22/2011

TOPOGRAPHIC RELIEF MAP of NYS. LANDFORMS of NYS. Landforms. Creation of NYS Landforms 9/22/2011 TOPOGRAPHIC RELIEF MAP of NYS LANDFORMS of NYS Prof. Anthony Grande AFG 2011 Landforms The basis of present-day landforms (surface features) is the bedrock geology that has been worked on by the forces

More information

2015: A YEAR IN REVIEW F.S. ANSLOW

2015: A YEAR IN REVIEW F.S. ANSLOW 2015: A YEAR IN REVIEW F.S. ANSLOW 1 INTRODUCTION Recently, three of the major centres for global climate monitoring determined with high confidence that 2015 was the warmest year on record, globally.

More information

Anthelia juratzkana Gymnomitrion corallioides Biological Crust Plant Association Liverwort Biological Crust Plant Association Southern Alaska

Anthelia juratzkana Gymnomitrion corallioides Biological Crust Plant Association Liverwort Biological Crust Plant Association Southern Alaska Anthelia juratzkana Gymnomitrion corallioides Biological Crust Plant Association Liverwort Biological Crust Plant Association Southern Alaska Conservation Status Rank: S4 (apparently secure) Introduction

More information

16 th Annual Invasive Species Workshop

16 th Annual Invasive Species Workshop 16 th Annual Invasive Species Workshop Predicting rapid expansion: What are the biological characteristics of Alaska s most invasive plant species? Flagstad, Lindsey A. 1, Justin R. Fulkerson 1, Casey

More information

Your 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 Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore CO NTINENTAL SHEL F For the complete encyclopedic entry with media

More information

Geology and Earth Resources

Geology and Earth Resources Geology and Earth Resources 1 A Layered Sphere Core dense, intensely hot metal! Mostly Fe and Ni! Inner and Outer Core Mantle - Hot, pliable layer, less dense! O 2, Si, Mg! Mesosphere (lower mantle)! Asthenosphere

More information

Climate.tgt, Version: 1 1

Climate.tgt, Version: 1 1 Name: Key Concepts Choose the letter of the best answer. (5 points each) 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. Date: A city located in the middle of North America experiences extreme temperature changes during

More information

Spheres of Life. Ecology. Chapter 52. Impact of Ecology as a Science. Ecology. Biotic Factors Competitors Predators / Parasites Food sources

Spheres of Life. Ecology. Chapter 52. Impact of Ecology as a Science. Ecology. Biotic Factors Competitors Predators / Parasites Food sources "Look again at that dot... That's here. That's home. That's us. On it everyone you love, everyone you know, everyone you ever heard of, every human being who ever was, lived out their lives. Ecology Chapter

More information

Surface Processes on the Earth. Rocks, Weathering, Erosion and Soil

Surface Processes on the Earth. Rocks, Weathering, Erosion and Soil Surface Processes on the Earth Rocks, Weathering, Erosion and Soil ROCKS AND ROCK CYCLE Rock types Three main types of rock Igneous Metamorphic Sedimentary Igneous Form when magma or lava cools and hardens

More information

Lab 7: Sedimentary Structures

Lab 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 information

Objectives. Introduction to Soils. Terms to know: What is soil? Study of Soils. The Soil Body 11/9/2012

Objectives. Introduction to Soils. Terms to know: What is soil? Study of Soils. The Soil Body 11/9/2012 Objectives Explain what soil is and where it comes from Define a soil body List examples of the five soil-forming factors Explain how soils develop Introduction to Soils Terms to know: What is soil? Alluvial

More information

Chapter 1 Section 2. Land, Water, and Climate

Chapter 1 Section 2. Land, Water, and Climate Chapter 1 Section 2 Land, Water, and Climate Vocabulary 1. Landforms- natural features of the Earth s land surface 2. Elevation- height above sea level 3. Relief- changes in height 4. Core- most inner

More information

Soil. Soil in Our Environment

Soil. Soil in Our Environment Soil Soil in Our Environment What is soil? Or is it Dirt? Gold s father is dirt, yet it regards itself as noble. Yiddish Proverb Is it alive? Is it fragile? Formations of Soils How much time does it take

More information

UNIT 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 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 information

River Response. Sediment Water Wood. Confinement. Bank material. Channel morphology. Valley slope. Riparian vegetation.

River Response. Sediment Water Wood. Confinement. Bank material. Channel morphology. Valley slope. Riparian vegetation. River Response River Response Sediment Water Wood Confinement Valley slope Channel morphology Bank material Flow obstructions Riparian vegetation climate catchment vegetation hydrological regime channel

More information

Geology of the Hawaiian Islands

Geology of the Hawaiian Islands Geology of the Hawaiian Islands Class 12 19 February 2004 A B C D F 97 94 92 91 88 87 86 85 85 84 82 77 73 73 mean 66 64 60 69 60 57 51 29 Exam Scores Mean = 71 Median = 82/77 Any Questions? Sedimentary

More information

Physiographic Provinces (West, Ch. 13)

Physiographic Provinces (West, Ch. 13) Geology 229 Engineering Geology Lecture 13 Physiographic Provinces (West, Ch. 13) The definition of the term Physiography Physiography (n.) The science which treats of the earth's exterior physical features,

More information

Ecosystems Chapter 4. What is an Ecosystem? Section 4-1

Ecosystems Chapter 4. What is an Ecosystem? Section 4-1 Ecosystems Chapter 4 What is an Ecosystem? Section 4-1 Ecosystems Key Idea: An ecosystem includes a community of organisms and their physical environment. A community is a group of various species that

More information

Soils and Soil Minerals. Remember, most things can be too little or too much.

Soils and Soil Minerals. Remember, most things can be too little or too much. Soils and Soil Minerals Remember, most things can be too little or too much. 1 2 3 Source of essential elements CO 2, O 2 from atmosphere H 2 0, O 2, minerals from soil NH 4, SO 4 can volatilize and be

More information

Weathering and Erosion

Weathering and Erosion Weathering and Erosion OBJECTIVE: Explain how erosion and deposition shape Earth s surface by matching and using models How do erosion and deposition shape Earth s surface? Deposition Formation Transported

More information

Lecture #14 March 29, 2010, Monday. Air Masses & Fronts

Lecture #14 March 29, 2010, Monday. Air Masses & Fronts Lecture #14 March 29, 2010, Monday Air Masses & Fronts General definitions air masses source regions fronts Air masses formation types Fronts formation types Air Masses General Definitions a large body

More information

Keys to Climate Climate Classification Low Latitude Climates Midlatitude Climates High Latitude Climates Highland Climates Our Changing Climate

Keys to Climate Climate Classification Low Latitude Climates Midlatitude Climates High Latitude Climates Highland Climates Our Changing Climate Climate Global Climates Keys to Climate Climate Classification Low Latitude Climates Midlatitude Climates High Latitude Climates Highland Climates Our Changing Climate Keys to Climate Climate the average

More information

Energy Systems, Structures and Processes Essential Standard: Analyze patterns of global climate change over time Learning Objective: Differentiate

Energy Systems, Structures and Processes Essential Standard: Analyze patterns of global climate change over time Learning Objective: Differentiate Energy Systems, Structures and Processes Essential Standard: Analyze patterns of global climate change over time Learning Objective: Differentiate between weather and climate Global Climate Focus Question

More information

WHAT IS THE EARTH MADE OF? LITHOSPHERE AND HYDROSPHERE

WHAT 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 information

Name. 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. 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 information

Adopt a Drifter Lesson Plan by Mary Cook, Middle School Science Teacher, Ahlf Jr. High School, Searcy, Arkansas

Adopt a Drifter Lesson Plan by Mary Cook, Middle School Science Teacher, Ahlf Jr. High School, Searcy, Arkansas Adopt a Drifter Lesson Plan by Mary Cook, Middle School Science Teacher, Ahlf Jr. High School, Searcy, Arkansas Do Ocean Surface Currents Influence Climate? Objectives Students will construct climographs

More information

Weather and Climate Summary and Forecast October 2018 Report

Weather and Climate Summary and Forecast October 2018 Report Weather and Climate Summary and Forecast October 2018 Report Gregory V. Jones Linfield College October 4, 2018 Summary: Much of Washington, Oregon, coastal California and the Bay Area and delta region

More information

Permafrost-influenced Geomorphic Processes

Permafrost-influenced Geomorphic Processes Section 4 Permafrost-influenced Geomorphic Processes Geomorphic processes vary greatly among ecoregions in northern Alaska, extending from the Beaufort Sea coast to the Brooks Range (Figure 4.1). Regional

More information

Which map shows the stream drainage pattern that most likely formed on the surface of this volcano? A) B)

Which map shows the stream drainage pattern that most likely formed on the surface of this volcano? A) B) 1. When snow cover on the land melts, the water will most likely become surface runoff if the land surface is A) frozen B) porous C) grass covered D) unconsolidated gravel Base your answers to questions

More information

Practice Questions for Lecture 5 Geology 1200

Practice Questions for Lecture 5 Geology 1200 Practice Questions for Lecture 5 Geology 1200 Use these questions to test your knowledge of Lecture5. The exams will be similar in format, except that they will deal with more than one chapter, and will

More information

Climate. What is climate? STUDY GUIDE FOR CONTENT MASTERY. Name Class Date

Climate. What is climate? STUDY GUIDE FOR CONTENT MASTERY. Name Class Date Climate SECTION 14.1 What is climate? In your textbook, read about climate and different types of climate data. Put a check ( ) next to the types of data that describe climate. 1. annual wind speed 4.

More information

The Great Ice Ages. Copyright abcteach.com 2001 Graphics from Art Today

The Great Ice Ages. Copyright abcteach.com 2001 Graphics from Art Today The Great Ice Ages The Great Ice Ages occurred during the Pleistocene epoch. The word epoch means time period. This period began about 2.5 million years ago and ended roughly 10,000 years ago. During the

More information

What is a landform? These shapes (except for bodies of water) on the earth s surface are all examples of landforms.

What is a landform? These shapes (except for bodies of water) on the earth s surface are all examples of landforms. Landforms What is a landform? These shapes (except for bodies of water) on the earth s surface are all examples of landforms. archipelago a large group of many islands. The Hawaiian Islands Lighthouse

More information

Oregon Water Conditions Report April 17, 2017

Oregon Water Conditions Report April 17, 2017 Oregon Water Conditions Report April 17, 2017 Mountain snowpack continues to maintain significant levels for mid-april. By late March, statewide snowpack had declined to 118 percent of normal after starting

More information

netw rks Guided Reading Activity Essential Question: How does geography influence the way people live? Earth's Physical Geography

netw rks Guided Reading Activity Essential Question: How does geography influence the way people live? Earth's Physical Geography Guided Reading Activity Lesson 1 Earth and the Sun Essential Question: How does geography influence the way people live? Looking at Earth Directions: What are the layers that make up Earth? Use your textbook

More information

ENVIRONMENTAL SCIENCE

ENVIRONMENTAL SCIENCE Advanced Placement ENVIRONMENTAL SCIENCE Geologic Processes & Soil Student 2014 Geologic Processes and Soil Geologic Processes The age of Earth is best measured by the geologic time scale. The idea that

More information

Classification according to patent rock material/origin, soil distribution and orders

Classification according to patent rock material/origin, soil distribution and orders Classification according to patent rock material/origin, soil distribution and orders Alluvial Soils Shales and Sandstone Soils Limestone Soils Chocolate Hills: Limestone formation Andesite and Basalt

More information

Unit 1: Geography. For additional information, refer to this website: 1 G e o g r a p h y

Unit 1: Geography. For additional information, refer to this website:  1 G e o g r a p h y Unit 1: Geography For additional information, refer to this website: http://mryoungtms.weebly.com/ 1 G e o g r a p h y Continents and Oceans SOL USI. 2a Essential Understanding: Continents are large land

More information

Physical Geography: Patterns, Processes, and Interactions, Grade 11, University/College Expectations

Physical Geography: Patterns, Processes, and Interactions, Grade 11, University/College Expectations Geographic Foundations: Space and Systems SSV.01 explain major theories of the origin and internal structure of the earth; Page 1 SSV.02 demonstrate an understanding of the principal features of the earth

More information

Lecture Outlines PowerPoint. Chapter 12 Earth Science 11e Tarbuck/Lutgens

Lecture Outlines PowerPoint. Chapter 12 Earth Science 11e Tarbuck/Lutgens Lecture Outlines PowerPoint Chapter 12 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors

More information

Changes in Texas Ecoregions

Changes in Texas Ecoregions Comment On Lesson Changes in Texas Ecoregions The state of Texas can be divided into 10 distinct areas based on unique combinations of vegetation, topography, landforms, wildlife, soil, rock, climate,

More information

ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE!

ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE! ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE! WHAT PROMINENT FEATURE CAN YOU IDENTIFY IN THIS PICTURE? What do you think the different colors represent? Who might find such a picture

More information

Hiking the Bold Coast, Cutler, Maine

Hiking 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 information

6.E E Rock Cycle/Weathering/Soil

6.E E Rock Cycle/Weathering/Soil Name: Date: 1. A lake is surrounded by hills covered with trees and shrubs. Which statement correctly describes how a change to the plants in this area will affect this environment? A. Adding plants to

More information