Young Naturalists Teachers Guide for the Glacier Did It
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Sophie's Ice Cream Cartopens PDF File
Connect your circuits to rPower* to control them remotely from a smartphone or tablet! Alice and Bettina became friends in their university’s master’s *Sold separately. engineering program, and soon discovered that they were both TM inspired to pursue engineering by childhood toys. To help inspire the We wanna hear about all the fun you had! Contact us at: Customer Service, 1400 E. Inman Pkwy., Beloit, WI 53511 • [email protected] • 1-800-524-4263. ® For more fun, visit playmonster.com Copyright © 2016 PlayMonster LLC, Beloit, WI 53511 USA. Made in China. All rights reserved. Roominate, The creative wired next generation of innovators, Alice and Bettina designed Roominate ! building kit and Switch on Your Imagination are trademarks of PlayMonster LLC. BUILD the Ice Cream Cart and a table! 2 Bonjour! I’m Sophie, and I can’t wait to see the ice cream cart you 1 design for me! ABOUT SOPHIE Favorite Activities: Cooking, reading and learning French Favorite Foods: Chicken noodle soup, cookies and ice cream Favorite Project: I have developed the best chocolate chip cookie recipe…it’s amazing how much chemistry is in cooking! Favorite Scientist: Dorothy Hodgkin Fun Fact: I’m planning to backpack in Europe after I graduate! I Want to Be: A chemist so I can design new medicine to help people, and discover ways for everyone to have clean water and healthy food! WIRE Collect all of the You can also add a motor to make it move! Sold separately. More designs at dolls, pets and roominatetoy.com! Roominate® kits! 1 2 Actual color of pieces in your set may be dierent from those shown here. -
WELLESLEY TRAILS Self-Guided Walk
WELLESLEY TRAILS Self-Guided Walk The Wellesley Trails Committee’s guided walks scheduled for spring 2021 are canceled due to Covid-19 restrictions. But… we encourage you to take a self-guided walk in the woods without us! (Masked and socially distanced from others outside your group, of course) Geologic Features Look for geological features noted in many of our Self-Guided Trail Walks. Featured here is a large rock polished by the glacier at Devil’s Slide, an esker in the Town Forest (pictured), and a kettle hole and glacial erratic at Kelly Memorial Park. Devil’s Slide 0.15 miles, 15 minutes Location and Parking Park along the road at the Devil’s Slide trailhead across the road from 9 Greenwood Road. Directions From the Hills Post Office on Washington Street, turn onto Cliff Road and follow for 0.4 mile. Turn left onto Cushing Road and follow as it winds around for 0.15 mile. Turn left onto Greenwood Road, and immediately on your left is the trailhead in patch of woods. Walk Description Follow the path for about 100 yards to a large rock called the Devil’s Slide. Take the path to the left and climb around the back of the rock to get to the top of the slide. Children like to try out the slide, which is well worn with use, but only if it is dry and not wet or icy! Devil’s Slide is one of the oldest rocks in Wellesley, more than 600,000,000 years old and is a diorite intrusion into granite rock. -
Model by Keven
High-quality constraints on the glacial isostatic adjustment process over North America: The ICE-7G_NA (VM7) model by Keven Roy A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Graduate Department of Physics University of Toronto © Copyright 2017 by Keven Roy Abstract High-quality constraints on the glacial isostatic adjustment process over North America: The ICE-7G_NA (VM7) model Keven Roy Doctor of Philosophy Graduate Department of Physics University of Toronto 2017 The Glacial Isostatic Adjustment (GIA) process describes the response of the Earth’s surface to variations in land ice cover. Models of the phenomenon, which is dominated by the influence of the Late Pleistocene cycle of glaciation and deglaciation, depend on two fundamental inputs: a history of ice-sheet loading and a model of the radial variation of mantle viscosity. Various geophysical observables enable us to test and refine these models. In this work, the impact of the GIA process on the rotational state of the planet will be analyzed, and new estimates of the long-term secular trend associated with the GIA process will be provided. It will be demonstrated that it has undertaken a significant change since the mid-1990s. Other important observables include the vast amount of geological inferences of past sea level change that exist for all the main coasts of the world. The U.S. Atlantic coast is a region of particular interest in this regard, due to the fact that data from the length of this coast provides a transect of the forebulge associated with the former Laurentide ice sheet. -
During the Last Ice Age As Ice Sheets Moved Southward Over Our Region, Glaciers Broke Off and Carried Pieces of the Underlying Bedrocks
“Glacial Erratics and Fieldstones” Boulders and other rocks broken off and carried by ice sheets covering this region were left in place when the glaciers melted. Geologists call these “erratics.”. Early settlers called them “fieldstones” and used them to build their house walls. During the last Ice Age as ice sheets moved southward over our region, glaciers broke off and carried pieces of the underlying bedrocks. When the ice melted, the fragments were left scattered over the surface. Geologists call such transported rocks “glacial erratics,” because they are different from the native bedrock. Most of these were pebble- and boulder-sized, mixed into sands and clay. A few are more than 10 feet high, such as Haring Rock in the Tenafly Nature Center (Fig 1A) and Tripod Rock in Sussex County (Fig. 1b). Fig. 2 shows images of erratics of various sized in a state park. As the ice sheets moved, rocks underneath often scratched parallel grooves in the bedrocks. These are called “glacial striations” (Fig. 3). Until Englewood Township was formally organized in 1859, most of what is now our City consisted of small farms which stretched from Overpeck Creek uphill to the Hudson River. Like other early European settlers, the farmers needed to move the boulders and other glacial erratics to create plowable fields. Rocks were gathered to build stone walls typical of New England and other glaciated parts of the Northeast. (Fig. 4). Many of the stones collected from the fields (“fieldstones”) were trimmed to make the walls of homes and other buildings. Many of the remaining buildings from the Dutch/English colonial period and the early 19th Century here in Englewood and vicinity incorporated “fieldstones” in their walls. -
Ice Cream Cone Pan 2105-2087
Instructions for To Decorate Ice Cream Cone Cake You will need Wilton Icing Colors in Ivory, Golden Yellow, Rose; Tips 3, Baking & Decorating 16; Wilton Rainbow Jimmies Sprinkle Decorations. We suggest you tint all icings at one time, while the cake cools. Refrigerate icing in covered Ice Cream Cone containers until ready to use. Make 3 cups buttercream icing: Cakes • Tint 1/4 cup dark Ivory/Golden Yellow combination • Tint 1 1/4 cups light Ivory/Golden Yellow combination PLEASE READ THROUGH INSTRUCTIONS BEFORE YOU BEGIN. • Tint 1 1/2 cups rose (thin with 1 Tablespoon + 1 1/2 teaspoons light IN ADDITION, to decorate cake you will need: corn syrup) • Wilton Decorating Bags and Couplers or Parchment WITH DARK IVORY/GOLDEN YELLOW ICING Triangles • Use tip 3 and “To Make Outlines” directions to outline waffle pattern on co n e • Tips 3, 16 • Wilton Icing Colors in Ivory, Golden Yellow, Rose WITH LIGHT IVORY/GOLDEN YELLOW ICING (alternate design uses Kelly Green) • Use tip 16 and “To Make Stars” directions to cover cone • Cake Board, Fanci-Foil Wrap or serving tray WITH THINNED ROSE ICING • One 2-layer cake mix or ingredients to make favorite • Use spatula to ice fluffy bottom scoop, then top scoop layer cake recipe Immediately sprinkle scoops with rainbow jimmies. • Buttercream Icing (recipe included) • Alternate designs use Chocolate Mousse and Chocolate Buttercream Icing (recipes included) or Wilton Chocolate Ready-To-Use Decorator Icing, Wilton Candy Melts® in Light Cocoa and Pink, Wilton Rainbow Nonpareils and Rainbow Jimmies Sprinkle Decorations, Wilton Vanilla Whipped Icing Mix, chocolate chips, red gumball, favorite crisped rice cereal treat recipe, vegetable pan spray, light corn syrup Wilton Method Cake Decorating Classes Iced fluffy with thinned rose Sprinkle with icing rainbow jimmies Call: 800-942-8881 © 2003 Wilton Industries, Inc. -
Let's Crank Some Ice Cream
Let’s Crank Some Ice Cream! The history of ice harvesting, the ice industry, refrigeration, and making ice cream Kathi Elkins 7-29-19 OLLI: Summer 2019 Ice Storage and Ice Houses: 1780 BC --- ice house in northern Mesopotamian 1100 BC --- evidence of ice pits in China By 400 BC --- Persian engineers had mastered techniques of constructing yakhchāl to store ice harvested from nearby mountains. 300 BC --- Alexander the Great (snow pits to hold snow and ice) 200s AD --- Romans (snow shops) Cold springs, root cellars Ice Houses: Yakhchāl (this one at Yazd, Iran) is a Persian ice pit or a type of evaporative cooler. Above ground, the structure had a domed shape, but had a subterranean storage space. It was often used to store ice and food. The subterranean space coupled with the thick heat-resistant construction material insulated the storage space all year. Ice Houses: Ice houses in England/UK. Ice Houses: Croome's thatched ice house, Worcestershire, UK Ice Houses: Botany Bay Icehouse, Edisto Island, SC Ice Houses: Ice house designs usually began as an underground egg-shaped cellar. This ice house, dating from 1780s and designed by architect John Nash, was discovered in 2018 buried under London streets. In 1822, following a very mild winter, William Leftwich chartered a vessel to Norway to collect 300 tons of ice harvested from crystal-clear frozen lakes. Previous imports had been lost at sea, or melted while baffled customs officials dithered over how to tax such unique cargo. John Nash designed the Royal Pavilion at Brighton, as well as Buckingham Palace. -
ICE CREAM MAKER Instruction Manual & Recipes
ICE CREAM MAKER Instruction Manual & Recipes MODEL: AIC-100 (Capacity: 1 Quart) Congratulations on your purchase of Aroma's Ice Cream Maker. It allows you to make your own rich and creamy HOMEMADE ice cream or frozen yogurt with the flip of a switch. You can also make your own favorite, healthy and delicious sherbet, sorbet, ice and frozen drinks fast and easy with Aroma Ice Cream Maker. Enjoy your new Ice Cream Maker, it is fun and easy! Please read all instructions carefully before using this product. Published By: Aroma Housewares Company 6469 Flanders Drive San Diego, CA 92121 U.S.A. ©2003 Aroma Housewares Company IMPORTANT SAFEGUARDS Basic safety precautions should always be followed when using electrical appliances, including the following: 1. Read all Instructions before using the appliance. 2. To protect against electrical hazard, do not immerse main body-the motor base or other electrical cord in water or other liquid. 3. Close supervision is necessary when any appliance is used by or near children. 4. Unplug appliance from outlet when not in use, before putting on or taking off parts and before cleaning. 5. Avoid contacting moving parts. Keep fingers, hair, clothing, as well as spatulas and other utensils away during operation. 6. Do not operate any appliance with a damaged cord or plug or after the appliance malfunctions or is dropped or has been damaged in any manner. Return appliance to the nearest authorized service facility for examination, repair or adjustment. 7. The use of accessory attachments not recommended by the appliance manufacturer may cause hazards. -
Daisy at Home Recipe for a Small Glacier
Daisy at Home Recipe for a Small Glacier Supplies Scientific Concepts • 1 pint of chocolate swirl or Glacier: A huge, thick sheet marble ice cream. of moving ice. They are often found in mountains, • 3 of your favorite kinds of cookies. but can be found in other places, too. Washington • 1/4 cup of light-colored was half covered in a syrup (butterscotch, glacier during the Ice Age! marshmallow, etc.) • Plastic sandwich bag or similar. Glacial till: Materials, such as rocks and dirt, left • A clear bowl. behind when a glacier • A spoon. melts. Most of the soil in the Seattle area is made of glacial till. Daisy at Home Recipe for a Small Glacier Instructions 1. Crumble up the cookies and put them in the bowl. This represents dirt and rocks that will become glacial till. 2. Put two big scoops of the ice cream on top of the crumbled cookies. Glaciers begin as clean snow and ice, but they pick up dirt and rocks from the ground as they travel. So, the ice cream with its swirls represents this “dirty” glacier! 3. Slide the plastic sandwich bag over your hand. Then, slowly push down or “smoosh” the ice cream so it oozes! What do you notice? What happens to the cookie crumbles? A glacier moves in a similar way. As more snow falls on it, the added weight causes the glacier to “ooze” or “flow,” pushing the dirt in all directions. 4. To see how glaciers flow, heat up your light-colored syrup and pour it over the ice cream. -
Gas Hydrates As a Functional Foaming Agent for Viscous Food Matrices
Research Collection Doctoral Thesis Gas Hydrates as a Functional Foaming Agent for Viscous Food Matrices Author(s): Šedivá, Zuzana Publication Date: 2019 Permanent Link: https://doi.org/10.3929/ethz-b-000352862 This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library Diss. ETH No. 25820 Gas hydrates as a functional foaming agent for viscous food matrices A dissertation submitted to attain the degree of DOCTOR OF SCIENCES of ETH ZURICH (Dr. sc. ETH Zurich) presented by Zuzana Šedivá MSc in Food Science ETH Zurich born 26th May 1987 citizen of Czech Republic accepted on the recommendation of Prof. Dr. E. J. Windhab, Examiner Dr. Martin Leser, Co-Examiner Dr. Vincent Meunier, Co-Examiner 2019 Summary A novel technology for foaming viscous slurries was designed. The process involved a crystalline gas hydrate dispersion as a functional ingredient standing in the core of the technology. Gas hydrates, also known as clathrate hydrates, are solid inclusion compounds, in which gas molecules are physically entrapped in a network of cavities made up of water molecules held together by hydrogen bonds (Marinhas et al., 2007). Gas hydrates exist at moderate pressures and low temperatures and possess a high volumetric gas storage capacity. The innovative idea of replacing highly energetically demanding foaming of viscous slurries using pure gas with the gas hydrate technology emerges in the current study. Introducing a gas as a slurry in its solid clathrate form into another viscous product stream reduces the energy input otherwise needed in powerful mixing devices. -
Science Lesson Plan
How Do Glaciers Scratch And Move Rocks? Purpose: Students will model the action of a rock-filled glacier with ice cubes and learn how glaciers can make scratches in Earths surface. Text: McGraw Hill, Pg. 175 Explore Activity McGraw Hill Science Journal, Pg. 75 Resources: I have added an additional experiment that you can do in your classroom after lab to reinforce the concepts being taught this week. Learning Outcomes: Students will discuss and know how glaciers scratch and move rocks. (Homeroom Teacher) Bridge-in: Share student’s hypothesis with class: How can a block of ice help shape the Earth’s surface? Prior Knowledge: How are icebergs formed? Do you think that a glacier is able to make scratches in the Earth’s surface? If YES, then HOW? If NO, then WHY? Input from you: Review what a prediction is. What is meant by using, the word, variable(s) in an experiment? What is an observation? What do I mean when I use the term inference? (Science Facilitator) Materials: Science Notebook Science Journal Pg. 75 Paper towels Clean ice cubes Ice cubes made with sand Aluminum foil Wood scraps, large enough to scrape ice cubes against. Guided Procedure: Predict: Which ice cube do you think is more like a real glacier? Record your prediction and reasons in your journal. Using Variables: Think about how you could use the materials to test your ideas. Which ice cube will scratch a surface? Record your observations for each ice cube. Observation: Which cube will leave “rocks” behind? Place the ice cubes on a folded paper towel. -
RECIPE for MAKING LIQUID NITROGEN ICE CREAM (Serves About 18-20 Students)
RECIPE FOR MAKING LIQUID NITROGEN ICE CREAM (serves about 18-20 students) NOTE: This is NOT a regular ChemDemo activity but rather a “treat” to go along with a regular ChemDemo 1. Add 1 quart Half and Half and 1 quart Heavy Whipping Cream into a large plastic or glass salad or punch bowl. 2. Add ¾ to 1 cup of granulated sugar (1 cup is a little on the sweet side). 3. 4-5 teaspoons of vanilla. 4. Optional: 1 pound of fresh fruit or preserves (not jelly). Strawberry or peach works best. If using fresh fruit, cut into small pieces. Chocolate syrup (8 oz) works well to make chocolate ice cream. If using chocolate syrup use less sugar (½ to ¾ cup). 5. Stir the mix for 2-3 minutes to dissolve the sugar. 6. Add about 2-3 liters of liquid nitrogen slowly and in small portions into the mix and stir with a wooden spoon. Pour a little at a time and stir; then continue adding small amounts of liquid nitrogen until you have the desired consistency. One person should be stirring while another gradually pours in the LN2. Another person may be necessary to hold the container when it starts getting thick. 7. Allow any excess liquid nitrogen to boil off. 8. Serve to your audience. Enough for 20 students (half a cup each). 9. Wash equipment and enjoy. SAFETY NOTE: LN2 is extremely cold (-196°C, -321°F, 77 K)!! Spilling it on you can cause serious frost- bite burns! Pouring some on unprotected skin is actually less dangerous than on clothing in contact with skin. -
The Early Wisconsinan History of the Laurentide Ice Sheet
Document généré le 30 sept. 2021 19:59 Géographie physique et Quaternaire The Early Wisconsinan History of the Laurentide Ice Sheet L’évolution de la calotte glaciaire laurentidienne au Wisconsinien inférieur Geschichte der laurentischen Eisdecke im frühen glazialen Wisconsin Jean-Serge Vincent et Victor K. Prest La calotte glaciaire laurentidienne Résumé de l'article The Laurentide Ice Sheet L'identification, surtout en périphérie de l'inlandsis, de dépôts glaciaires que Volume 41, numéro 2, 1987 l'on croit postérieurs à la mise en place de sédiments non glaciaires ou de paléosols datant de l'interglaciaire sangamonien (phase 5) et antérieurs aux URI : https://id.erudit.org/iderudit/032679ar sédiments non glaciaires ou des sols mis en place au Wisconsinien moyen DOI : https://doi.org/10.7202/032679ar (phase 3) a amené de nombreux chercheurs à supposer que la calotte laurentidienne s'est d'abord développée au Sangamonien ou au Wisconsinien inférieur (phase 4). On passe en revue les différentes preuves associées au Aller au sommaire du numéro début de la formation de la calotte glaciaire wisconsinienne recueillies au Canada et au nord des États-Unis. En l'absence quasi généralisée de données géochronométriques sûres pour déterminer l'âge des dépôts glaciaires datant Éditeur(s) probablement du Sangamonien ou du Wisconsinien inférieur, on peut aussi bien supposer, pour une période donnée, que les glaces ont entièrement envahi Les Presses de l'Université de Montréal une région ou en étaient tout à fait absentes. En tenant pour acquis (?) que la calotte laurentidienne était en fait très étendue au Wisconsinien inférieur, on ISSN présente une carte montrant son étendue maximale et un tableau de 0705-7199 (imprimé) corrélation entre les unités glaciaires.