Energy Transfer Worksheet
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The document is a worksheet that provides examples of different types of energy transfer - conduction, convection, and radiation. Students are asked to identify each example as one of the three types of energy transfer. They are also asked questions about diagrams showing temperature differences and how convection currents would flow between areas.
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This document is a note packet about plate tectonics, earthquakes, and volcanoes for an Earth Science class. It includes vocabulary words and information about plate tectonics theory, evidence for seafloor spreading, types of plate boundaries and plate motions, mantle convection cells, and hot spots. The packet contains diagrams and questions to help students understand key concepts about the dynamic nature of the Earth's interior and crust.
Grade 4 ns activity
The documents discuss states of matter, changes of state through various processes like melting and evaporation, and the water cycle. It also discusses how paper is manufactured from wood pulp and describes experiments on strengthening materials like investigating different pillar shapes and making paper struts. The final summary discusses designing, making and evaluating strong structures using tubular paper struts.
1st Summative Test Q2.docx
1. This document appears to be a summative test on environmental science topics for junior high school students.
2. The test covers identification questions on different types of rocks, ecological succession concepts, and sequencing primary succession stages.
3. It asks students to identify igneous rocks, sedimentary rocks, metamorphic rocks, erosion, weathering, lava, magma, compaction, pioneer species, primary succession, secondary succession, climax community, and ecological succession.
Earth and Life Science Quiz #1.docx
1. The document is a quiz on earth and life science that covers topics on the origin of the universe, planetary formation, and characteristics of the solar system.
2. Questions 1-10 cover identification of terms related to cosmology, geology, and astronomy.
3. Questions 11-20 involve multiple choice and ordering the planets from the sun. The final questions ask for explanations of the most acceptable theory of the origin of the universe and why Earth is considered a special planet.
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More from West Hollow MS Ms. Gill
Welcome to Regents Earth Science
This document provides instructions for students on the first day of an Earth Science class. It includes directions for students to find and label their seat, make a name tag, and fill out an index card with personal information. The document outlines classroom rules and procedures, such as arriving on time, respecting others, and asking permission to move around the room. It also lists required class supplies, provides an overview of the units that will be covered during the year, and describes homework, lab, quiz, and test grading policies. General lab safety rules are outlined.
Syllabus earth science
This document is an Earth Science syllabus that outlines the course details and expectations for students. The syllabus introduces Ms. Gill as the teacher and describes the course as a challenging but fun Regents-level class. It provides supplies needed, resources available to students, the curriculum topics that will be covered over the year, basic class rules, and the grading policy. It emphasizes the importance of organization, hard work, and asking questions to succeed. Parents are asked to review the syllabus and return the signed bottom portion.
Prologue pp1 2012
This document provides an introduction to key concepts in science including observation, inference, prediction, classification, measurement, the metric system, rounding, and scientific notation. It discusses observational skills and how scientists make inferences, predictions, and classifications. It also covers measurement units and conversions, rounding procedures, and how to write numbers in scientific notation. The overall document serves as an overview of foundational scientific thinking and processes.
Prologue np1 2012
The document provides an introduction and overview for a science class. It includes definitions and examples of key science concepts like observation, inference, prediction, classification, measurement, mass, temperature, states of matter, and scientific notation. The summary also notes vocabulary terms that will be covered. Overall, the document outlines foundational science concepts and vocabulary to prepare students for the upcoming class.
Geologic History Note Packet
This document is a note packet for a unit on geologic history from an Earth Science class. It includes vocabulary words and concepts related to relative dating techniques, the geologic time scale, fossil records, evolution of life on Earth, and absolute dating using radioactive isotopes. Key events covered are the formation of Earth and development of its atmosphere, variations and evolution of life forms through geologic time as evidenced by fossils, and methods for correlating and dating rock layers both relatively and absolutely.
Geologic History Powerpoint Notes
The document summarizes Earth's geologic history condensed into one calendar year. Key events include:
- By March, oceans formed but no life existed on the barren planet.
- First life emerged in April in the form of single-celled organisms near ocean vents.
- By December, more complex sea creatures evolved and the first plants colonized land despite heavy rains.
- On December 31st, early humans appeared in the last hour of the year along with Neanderthals and cave drawings. Modern civilizations emerged in the final minutes.
Earthquakes final
The document discusses dynamics of the Earth's crust and evidence of its motion over time. It provides examples of marine fossils found in high elevations as evidence of crustal uplift. Sedimentary layers deposited horizontally also indicate regions were once under water. Earthquakes provide direct evidence of crustal movement through effects like fault lines and changes in land elevation recorded after quakes.
Earthquakes final
The document discusses dynamics of the Earth including evidence of crustal motions such as uplift and erosion that create mountains and sedimentary layers. It explains how marine fossils found in high elevations provide evidence of crustal movement over time. Earthquakes are described as being caused by the movement of tectonic plates and release of stress that builds in rocks, sending seismic waves that can be used to locate an earthquake's epicenter. The layers of the Earth are also outlined, with the crust varying in thickness and composition in different regions.
Plates ex2
The document is a plate tectonics exercise that asks students to calculate how far the Eurasian Plate will move in different time periods based on its rate of movement of 3 cm per year. It asks the direction the plate is moving, and then has the student calculate the distance after 100 years (300 cm), 1,000 years (3,000 cm), 1 million years (3,000,000 cm), and 1 billion years (30,000,000,000 cm).
Plates Lab
The document discusses the theory of the ancient supercontinent Pangea, which existed around 250 million years ago. All the continents were joined together in a "C" shape with a central sea called Tethys. Pangea's massive size meant dry inland areas and allowed animals to migrate between poles. The exercise has students cut out continents and try reconstructing Pangea, comparing their results to the provided reconstruction. Additional evidence like matching fossils and rock sequences between continents that were once joined supports the supercontinent theory.
Oceans and Basin Do Now
This document provides directions for students to label features on maps and cross-section profiles, including the mid-atlantic ridge, subduction zones, trenches, and areas of youngest, oldest, and continental crust. Students are asked to draw a line indicating sea level and label identifiable geological features.
Pangaea lab
This document provides instructions for an investigation into Alfred Wegener's theory of continental drift and the existence of the supercontinent Pangaea. Students are asked to cut out continents from a page of "continental pieces" and fit them together based on matching boundaries, fossils, and glacial patterns to recreate Pangaea, as Wegener had done using available evidence. They are then to glue the recreated continents and a key to a separate piece of paper and answer questions about which continents fit together best and other evidence that could support the existence of Pangaea.
Ocean bottom profiles
This document provides instructions for a classroom activity where students will label ocean basin features on three profiles and maps. Students are asked to match maps with profiles, draw a line indicating sea level, and label landforms and ocean zones. They also answer questions about crust types and relative depths. The activity aims to teach students about the structure of ocean basins through hands-on labeling and mapping.
Global Tectonic Plates HW
This document contains a worksheet for students to answer questions about tectonic plates based on a map on the back of the sheet. The questions ask students to identify different types of plate boundaries based on line thickness on the map, features characteristic of convergent and divergent boundaries, plates framed by convergent boundaries, specific plate boundaries, and distances between continental plates.
Earths Interior Questions HW
The document is a worksheet containing 11 multiple choice questions about the properties of Earth's interior layers based on a diagram. The questions ask about how temperature and pressure change with depth, the depth of boundaries between layers, observed temperatures, melting points, densities, compositions, and phases of the different layers.
Dynamic Earth
The document summarizes the structure and composition of Earth's interior. It has four main layers from innermost to outermost - the solid inner core made of iron and nickel, the liquid outer core also made of iron and nickel, the solid mantle made of iron, silicon and magnesium minerals, and the rigid outer crust made of lighter rock. Temperature and pressure increase from the crust towards the core. The crust is thinnest under oceans and thickest under mountains.
Earths dimension sci 8 ppt np1
This document provides information about Earth's spheres and mapping locations on Earth. It discusses the geosphere, atmosphere, hydrosphere, and biosphere. It describes latitude and longitude and how they are used in a coordinate system to locate positions on Earth. It also covers topics like time zones, topographic maps, and drawing contour lines.
Metamorphic Rocks
Metamorphic rocks are formed from existing rocks through recrystallization caused by heat and pressure, without melting. There are two types of metamorphism: regional metamorphism occurs over large areas with extreme heat and pressure, as in mountain building; contact metamorphism occurs only near intrusions and does not melt the rock. During metamorphism, new mineral crystals form and original structures can be distorted, resulting in foliated rocks like schist. Limestone becomes marble, sandstone becomes quartzite, and shale becomes slate through metamorphism. Fossils are not found in metamorphic rocks as the heat and pressure would destroy them.
Igneous Rocks
Rocks are classified based on how they form. The three main types are igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling and solidification of molten rock, either below the surface as intrusions or above the surface as extrusions. Texture and mineral composition are used to classify igneous rocks. Slow cooling forms large crystals while fast cooling forms small or no crystals. Sedimentary rocks form from the compaction or cementation of sediments. Metamorphic rocks form from changes to existing rocks via heat, pressure, and chemical reactions in the Earth.
Sedimentary rocks of the esrt
The document provides information about sedimentary rocks from a student worksheet, including particle size ranges for different sediments like sand and silt. It also details the minimum water velocities needed to transport different particle sizes, from pebbles to cobbles to boulders. Finally, it identifies the sedimentary rocks that form from the lithification of different sediments, such as silt becoming shale and sand becoming sandstone.
More from West Hollow MS Ms. Gill (20)
Energy Transfer Worksheet
- 1. Name: _________________________ Period:______ Date:________________<br />Unit 1: Energy Energy Transfer Worksheet<br />Directions: Identify the following as conduction, convection or radiation.<br />1. __________________: Heated air rises through earth’s atmosphere.<br />2. __________________: An ice cube melts when dropped into a glass of warm water.<br />3. __________________: Light leaves the sun and 8 minutes later strikes earth.<br />4. __________________: You burn you tongue eating hot pizza.<br />5. __________________: Hot magma rises inside earth’s mantle, cool, and sinks.<br />6. __________________: A microwave oven heats soup.<br />7. __________________: A fireplace warming a room.<br />The diagram below represents temperatures in degrees Celsius for a particular room:<br />28262423A26262423B26252422<br />8. Draw an arrow to show the direction of air movement between A and B.<br />9. Like energy will totally move from areas of ______________ to _______________.<br />0151765<br />Djflkdf<br />513282536190571500025311102971800253111010. The diagrams below represent beakers being heated by a Bunsen burner. Draw in arrows to show how convection will move in each beaker.<br />