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Glacier Facts & Worksheets

Glacier is an enduring body of thick ice that moves under its weight and forms when the accumulation of snow over many years, perhaps millennia, surpasses its ablation., search for worksheets, download the glacier facts & worksheets.

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Table of Contents

A glacier is an enduring body of thick ice that moves under its weight. A glacier formed when the accumulation of snow over many years, perhaps millennia, surpasses its ablation. As it slowly flows and deforms under the strains caused by its weight, it develops unique characteristics such as crevasses and seracs. It moves, abrading rock and debris from its substrate to generate landforms like cirques, moraines, and fjords. A glacier may float into a body of water, but it forms solely on land, as opposed to the much thinner sea ice and lake ice that develops on the surface of bodies of water .

See the fact file below for more information about Glacier, or download the comprehensive worksheet pack, which contains over 11 worksheets and can be used in the classroom or homeschooling environment.

Key Facts & Information

  • The term glacier is a foreign word from French and may be traced back to the Vulgar Latin via Franco-Provençal.
  • Latin glacirium , from Late Latin glacia , and Latin glacis , meaning “ice.”
  • Glacial processes and characteristics are those induced or influenced by glaciers. Glaciation is the process of glacier formation, development, and flow. 
  • Glaciology is a comparable field of study, and glaciers play a vital role in the global cryosphere.

CLASSIFICATION: SIZE, SHAPES, AND BEHAVIOR

  • Glaciers are classified based on their form, thermal properties, and behavior. Alpine glaciers grow on mountain crests and slopes. Valley glaciers, also known as alpine glacier, is a glacier that fills a valley. An ice cap or field is a vast body of glacial ice that sits atop a mountain range or volcano .
  • Ice caps cover less than 50,000 km2 (19,000 sq mi). Ice sheets or continental glaciers are glacial masses greater than 50,000 km2 (19,000 sq mi). They are many kilometers deep and hide the underlying landscape. Nunataks are the only things that protrude from their surfaces. The only remaining ice sheets are those that cover the majority of Antarctica and Greenland .
  • They hold so much freshwater that if both dissolved, global sea levels would increase by more than 70 meters (230 ft). Ice shelves are pieces of an ice sheet or cap that extend into the ocean; they are typically narrow, with restricted slopes and velocities. Ice streams are limited, fast-moving parts of an ice sheet.
  • Many ice streams in Antarctica flow onto enormous ice shelves. Some, like Mertz Glacier, drain directly into the sea, frequently with an ice tongue.
  • Many glaciers moving from Greenland, Antarctica, Baffin, Devon, and Ellesmere Islands in Canada , Southeast Alaska , and the Northern and Southern Patagonian Ice Fields are tidewater glaciers.
  • As the ice hits the sea, parts break off or calve, forming icebergs. Most tidewater glaciers calve above sea level, resulting in a massive impact as the iceberg strikes the water. Tidewater glaciers rise and retreat through centuries-long cycles that are far less impacted by climate change than other glaciers.

CLASSIFICATION: THERMAL STATE

  • A temperate glacier melts throughout the year, from its surface to its base. Polar glacier ice is constantly below the freezing point from the surface to the bottom, while the surface snowpack may melt seasonally.
  • A subpolar glacier contains both temperate and polar ice, depending on its depth under the surface and location along its length. Similarly, a glacier’s thermal regime is frequently defined by its basal temperature.
  • A cold-based glacier has an ice-ground contact below freezing and is frozen to the underlying substrate.
  • A warm-based glacier is above or near freezing at the interface and can slide there. This disparity is assumed to regulate a glacier’s capacity to successfully erode its bed since moving ice encourages tugging at the rock from the surface below.
  • Polythermal glaciers are those that are partially cold and partly warm.
  • Glaciers arise when snow and ice buildup surpass ablation.

A glacier is frequently formed by a cirque landform (also known as a “corrie” or a “cwm”), which is a characteristically armchair-shaped geological feature (such as a dip between mountains enclosed by arêtes) that accumulates and compresses the snow that falls into it by gravity.

  • This snow collects, and the weight of the snow falling compacts above it, resulting in the formation of névé (powdery snow).
  • Crushing the tiny snowflakes and squeezing the air out of the snow further transforms it into “glacial ice.” This glacial ice will cover the cirque until it “overflows” via a geological void or weakness, such as a breach between two mountains. When a pile of snow and ice becomes thick enough, it starts to move due to various surface slopes, gravity, and pressure.
  • It can happen on steeper slopes with as little as 15 m (50 ft) of snow-ice. Snow continually freezes and thaws in temperate glaciers, transforming into granular ice known as firn. This fine ice combines into denser firn under the weight of the layers of ice and snow above it.
  • Over time, firn layers grow more compacted and eventually turn into glacial ice. Because glacier ice has fewer trapped air bubbles, it is somewhat denser than ice created from frozen water.
  • Glacial ice is blue because it collects red light due to an overtone of the water molecule ‘s infrared OH stretching mode. (For the same reason, liquid water appears blue; the blue of glacier ice is frequently falsely attributed to Rayleigh’s scattering of bubbles in the ice.)
  • A glacier begins at a position known as the glacier head and ends at the glacier foot, snout, or terminal.
  • Glaciers are classified according to their surface snowpack and melt conditions. The ablation zone is the glacier area with a net mass loss, and the accumulation zone is the highest section of a glacier when accumulation surpasses ablation. The equilibrium line is the contour that divides the ablation zone from the accumulation zone; it is the contour where the quantity of fresh snow obtained by accumulation equals the amount of ice lost by ablation.
  • In general, the buildup zone accounts for 60-70% of the glacier’s surface area, with the accumulation zone accounting for even more of the glacier calves icebergs. The accumulation zone’s ice is deep enough to impose a downward pull on the underlying rock.
  • When a glacier melts, it frequently leaves behind a bowl- or amphitheater-shaped depression ranging in size from enormous basins like the Great Lakes to tiny mountain depressions known as cirques.
  • Can use the melt conditions of the accumulation zone to partition it.
  • The dry snow zone is characterized as a place with no melt, even during the summer, and a dry snowfall.
  • The percolation zone is a region with a surface melt that allows meltwater to seep into the snowpack. This zone is frequently distinguished by refrozen ice lenses, glands, and layers. Similarly, the snowpack never reaches the melting point.
  • A superimposed ice zone forms around the equilibrium line on some glaciers. Meltwater in the glacier refreezes as a cool layer, resulting in a persistent ice mass in this zone.
  • The wet snow zone is where all of the snow that has fallen since the end of the previous summer has reached 0 °C.
  • A glacier’s health is often determined by estimating the glacier mass balance or watching terminal activity. Healthy glaciers feature vast accumulation zones, more than 60% of their area is snow-covered after the melt season, and a vigorously flowing terminal.
  • Glaciers have receded significantly since the end of the Little Ice Age, about 1850. Between 1950 and 1985, a slight cooling caused many alpine glaciers to advance, but after 1985, glacier retreat and mass loss became more significant and widespread.
  • Glaciers migrate or flow downwards due to gravity and internal ice deformation. Ice acts like a brittle solid until its thickness surpasses around 50 m (160 ft). Plastic flow is caused by pressure on ice deeper than 50 meters. 
  • Ice comprises stacked layers of molecules with relatively weak connections at the molecular level. The layer above moves faster than the layer below when the load on the layer above surpasses the inter-layer binding strength.
  • Glaciers move with basal sliding as well. A glacier glides across the land it resides on, lubricated by the existence of liquid water. The water is formed when the ice melts under high pressure due to frictional heating. In temperate or warm-based glaciers, basal sliding is prevalent.

FRACTURE ZONE AND CRACKS

  • Because of the low pressure, the glacier’s top 50 meters (160 feet) are stiff. The fracture zone is the upper part, which travels primarily as a single unit over the plastic-flowing bottom segment. 
  • Crevasses form in the fracture zone of a glacier when it advances across uneven terrain—variations in glacier velocity cause crevasses to develop. Shear pressure causes two stiff portions of a glacier to break apart and open a crack if they move at opposite rates or orientations.
  • Crevasses are rarely more than 46 m (150 ft) deep but can be at least 300 m (1,000 ft) deep in extreme situations. The flexibility of the ice under this point prevents fissures from forming. Intersecting crevasses can form solitary ice peaks known as seracs.
  • Friction influences the pace of glacial movement, and friction causes the ice at the glacier’s bottom to move more slowly than at the glacier’s top. Friction is also formed along the valley’s sidewalls in alpine glaciers, slowing the margins relative to the center.
  • The average glacial pace varies widely, although it is usually approximately 1 meter (3 feet) daily. In static locations, there may be little movement; for example, trees can sustain themselves on surface sediment deposits in portions of Alaska. Other glaciers, such as Greenland’s Jakobshavn Isbrae, can flow as quickly as 20-30 m (70-100 ft) each day.
  • Slope, ice thickness, precipitation, longitudinal confinement, baseline temperature, meltwater production, and bed hardness all influence glacial pace.
  • Surges are episodes of swift progress on a few glaciers. These glaciers typically travel until they suddenly accelerate and then revert to their former movement condition. 
  • The breakdown of the underlying bedrock might trigger these surges, the pooling of meltwater at the glacier’s base — possibly delivered from a supraglacial lake — or simply the accumulation of mass beyond a crucial “tipping point.”
  • Ogives (or Forbes bands) are recurring wave crests and troughs that show on glacier surfaces as dark and light ice bands. They are related to seasonal glacier motion; the breadth of one dark and one bright band roughly reflects the glacier’s yearly movement. 
  • When ice from an icefall is badly broken up, it increases the ablation surface area throughout the summer. It provides a swale and room for snow accumulation in the winter, leading to a ridge formation. Ogives merely undulations or color bands are called wave ogives or band ogives.

CLIMATE CHANGE

  • Glaciers are essential for detecting long-term climate change since they can be hundreds of thousands of years old.
  • Ice cores are extracted to investigate the patterns throughout time in glaciers, giving frequent feedback, including evidence for climate change stored in the ice for scientists to break down and analyze. Glaciers are examined to understand the history of climate change caused by natural or human factors.
  • Human activity has generated a rise in greenhouse gases, resulting in global warming and the melting of these crucial glaciers. Glaciers have an albedo impact, and melting glaciers result in reduced albedo. Compared to the summer of 2003 in the Alps to the summer of 1988, the albedo value in 2003 was 0.2 lower than in 1998.
  • When glaciers melt, sea levels rise, “which increases coastal erosion and boosts storm surge as warmer air and ocean temperatures generate more frequent and stronger coastal storms like hurricanes and typhoons.”
  • Thus, human-caused climate change generates a positive feedback loop with glaciers: rising temperatures drive more glacier melt, resulting in less albedo, higher sea levels, and a slew of other climatic challenges.
  • NASA has employed a Landsat satellite to record glaciers in Alaska, Greenland, and Antarctica since 1972 and will persist until 2019. This Landsat project discovered that glacier retreat had risen significantly since roughly 2000.

Glacier Worksheets

This bundle contains 11   ready-to-use Glacier Worksheets that are perfect for students who want to learn more about a Glacier, which is an enduring body of thick ice that moves under its weight and forms when the accumulation of snow over many years, perhaps millennia, surpasses its ablation.

Download includes the following worksheets:

  • Glacier Facts
  • Glacier Sketch
  • Glacier Yes Or No
  • Glacier Acrostic Poem
  • Glacier Formation
  • Glacier Fill In The Blanks
  • Spot The Glaciers
  • Animals In Glaciers
  • All About The Titanic
  • Glacier News Report
  • Glacier Word Search

Frequently Asked Questions

What is a glacier.

A glacier is an enduring body of thick ice that moves under its weight. 

How does a glacier get its name?

The term glacier is a foreign word from French and may be traced back to the Vulgar Latin via Franco-Provençal. Latin glacirium , from Late Latin glacia , and Latin glacis , meaning “ice.”

How does glacier forms?

Why is glacier ice blue.

Glacial ice is blue because it collects red light due to an overtone of the water molecule’s infrared OH stretching mode.

How does climate change affect glaciers? 

When glaciers melt, sea levels rise, “which increases coastal erosion and boosts storm surge as warmer air and ocean temperatures generate more frequent and stronger coastal storms like hurricanes and typhoons.” Thus, human-caused climate change generates a positive feedback loop with glaciers: rising temperatures drive more glacier melt, resulting in less albedo, higher sea levels, and a slew of other climatic challenges.

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TRENDING TOPICS

Evidence found in himalayas reveals half of earth's glaciers will disappear if..., the research, published in the journal science, is based on extensive fieldwork conducted between 2013 to 2017 at the imja-lhotse shar glacier in the himalayas..

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Himalayan glacier

  • World's glaciers could lose as much as 40% of their mass
  • The study used sophisticated modeling techniques
  • The research is published in the journal Science

In a groundbreaking study led by Dr. David Rounce, assistant professor at Carnegie Mellon University, it has been estimated that the world's glaciers could lose as much as 40% of their mass by 2100 due to global warming.

The research, published in the journal Science , is based on extensive fieldwork conducted by Rounce and his team from 2013 to 2017 at the Imja-Lhotse Shar Glacier in the Himalayas.

Rounce's firsthand experience of the rapid recession of the glacier and the expansion of the lake at its base was a stark revelation of the effects of climate change. "To go to the same place and to see the lake expand and see how the glacier was thinning rapidly was quite eye-opening to say the least," Rounce said.

HImalayas

The study is the first of its kind to use satellite-derived mass change data describing all the world's 215,000 glaciers. The model accounted for glacial debris cover, which can influence glacial melting. A thin layer of debris can enhance melting, while a thick layer can insulate and reduce it.

Glaciers in remote regions, far from human activities, are particularly potent indicators of climate change. Their rapid melting impacts freshwater availability, landscapes, tourism, ecosystems, the frequency and severity of hazards, and sea level rise.

"Sea level rise is not just a problem for a few specific locations," said Ben Hamlington, leader of NASA's Sea Level Change Team. "It’s increasing almost everywhere on Earth."

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September 6, 2023 dialog

This article has been reviewed according to Science X's editorial process and policies . Editors have highlighted the following attributes while ensuring the content's credibility:

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Unraveling a paradox of Himalayan glacier melt

by Ryan M. Strickland

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Englacial insights

Journal information: Geophysical Research Letters

Ryan Strickland is a PhD student at the University of Arkansas in Fayetteville. His current research combines numerical modeling with expedition field work in the Himalaya and Alaska to better understand the evolution of debris-covered glaciers.

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Easy Science For Kids

Glaciers Worksheet – Free Science Kids Hidden Words Game Printable

Glaciers Quiz

The Glaciers Worksheet – Download our fun FREE science kids hidden words game printable worksheet. This free printable worksheet all about Glaciers for kids has a fun word seek game along with a find-the-hidden-and-missing words puzzle.

This science kids words game is free to download and print at no cost. Our fun facts on Glaciers worksheet is enjoyable for kids in Grammar school in 1st Grade to 5th Grade as well as for younger kids in Kindergarten and Pre-K kids.

This science kids hidden words game about Glaciers is a fun way to interest your child in science and gain your child’s interest during after school science classes or homeschooling science lessons. Children interested in learning about the world will have fun playing the word puzzle game while learning fun facts all about Glaciers.

Grade school kids from First Grade to Fifth Grade can use this free printable Glaciers worksheet as a reading comprehension worksheet. Children shall learn well about Glaciers, as they will most likely need to read a few times the fun facts about Glaciers to find all the missing words.  This exercise will not only improve children’s skills to remember what they read but also enhance their reading skills.

Kindergarten and Preschool kids who don’t yet know how to read can use this free Glaciers fun facts worksheet as an interesting listening comprehension game.

Teachers or Educators can read the all about Glaciers fun facts and then ask the children to recall what the missing words were.  Kindergarten & Pre-K kids can also enjoy playing the hidden words puzzle while learning to find and recognize letters and words.

Parents can use our fun facts about Glaciers for kids worksheet to do fun homeschooling or early learning science activities with their kids and spend quality time educating their kids about Glaciers. If your kid is enjoying home-schooling, or is enrolled in some extra-curricular program, then this is a fun science activity, with reading comprehension benefits for kids in grades one to five.

Teachers can use this free kids hidden words game to engage kids interest during science classes and to make learning facts about Glaciers interesting for kids.

Tutors can use our Glaciers free science hidden words game for extra-curricular science lessons or child enrichment programs.

Our fun facts on science for kids website offers many free science kids hidden words games and free science printable worksheets for kids. Download and use our fun science word puzzles to make learning science a fun experience for your kids!

What makes a Glacier form? Glaciers occur when the  snow falls faster than it can melt.

Learn more fun facts about Glaciers by downloading this free science kids Glaciers worksheet!

Free Printable Glaciers Worksheet for Kids

[sociallocker] Download our FREE science kids hidden words game about Glaciers .

Download the FREE Glaciers Worksheet for Kids!

Did you enjoy the FREE Glaciers Worksheet for Kids ? Read lengthy facts about Glaciers here .

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Hands-on Lessons and Activities about Glaciers

Glaciers can be a difficult subject to teach. Most students haven’t ever seen one. Furthermore, glaciers’ size and relatively slow rate of change make it difficult to understand how they can change the surface of the earth. Images from online galleries and children’s literature can help students begin to visualize these massive bodies of ice. Creating models will help them develop a basic understanding of the scientific principles at work in glacial formation , movement , and erosion . While many of these lessons are written for the upper elementary grades, teachers of primary students may be able to modify them by performing demonstrations rather than investigations.

Many of these lessons and activities lend themselves to making predictions, so we’ve chosen to highlight that strategy as our literacy integration . Students become proficient readers by making predictions and evaluating them based on the text, much in the same way that proficient scientists make predictions and evaluate based on experimental data. You may choose to have students record predictions on a worksheet or in a journal, or record their oral predictions as you discuss the experiment or text.

GLACIAL FORMATION

How Do Snowflakes Become Ice? (Grades K-5) Students model the formation of ice with marshmallows or, if it is available, snow. Lesson extensions suggest using snow cones or shaved ice to model the difference between snow, firn (an intermediate stage between snow and ice), and glacial ice. This lesson meets the National Science Education Standards : Science as Inquiry Content Standard, the Physical Science Content Standard, the Earth and Space Science Content Standard, and the History and Nature of Science Content Standard.

Glacial Pressure (Grades 3-5) In this lesson plan, students model glacial formation through the compression of marshmallows, which represent snow. Students observe the effect of pressure exerted on marshmallows and draw conclusions about pressure exerted on snow.

This lesson meets the National Science Education Standards : Science as Inquiry Content Standard and the Earth and Space Science Content Standard.

GLACIAL MOVEMENT

Blue Ice Cube Melt (Grades K-5) Students experiment with blue-colored ice cubes and learn that ice can melt under pressure. This lesson meets the National Science Education Standards : Science as Inquiry Content Standard, the Physical Science Content Standard, the Earth and Space Science Content Standard, and the History and Nature of Science Content Standard.

Modeling Glacier Dynamics with Flubber (Grades 2-3) Modeling Glacier Dynamics with Flubber (Grades 3-5)

These hands-on activities simulate glacial flow. The students use a glacier-modeling compound made from glue, water, and detergent (“flubber”) to predict and observe glacial flow. The students discuss with the teacher how scientists determine glacial flow with real glaciers. The link opens a zipped file that contains three documents: the teacher’s guide, notes, and a worksheet.

This unit meets the National Science Education Standards : Science as Inquiry Content Standard and the Earth and Space Science Content Standard.

GLACIAL EROSION

Explaining Glaciers, Accurately (Grades 3-5) This article from the National Science Teachers Association journal Science and Children describes two activities that help students develop correct understanding of how glaciers change the earth’s surface by plucking and abrasion. Free for NSTA members and nonmembers.

This lesson meets the National Science Education Standards : Earth and Space Science Content Standard.

INTEGRATING LITERACY

Use the books in this month’s Virtual Bookshelf and our Feature Story to help your students practice making predictions while reading!

It Doesn’t Have to End That Way: Using Prediction Strategies with Literature (Grades K-2) Primary students listen to the beginning of a story, and then use details in the text and prior knowledge to predict the way the story will end.

This lesson meets the following NCTE/IRA standards: 3, 4, 11, 12 .

Using Prediction as a Prereading Strategy (Grades 3-5) This three part lesson includes teacher modeling, guided practice, and independent practice with response journals. The lesson uses fiction trade books, but the approach can be used with any text or content area.

This activity meets the following NCTE/IRA standards: 3, 5 .

This article was written by Jessica Fries-Gaither. For more information, see the Contributors page. Email Kimberly Lightle , Principal Investigator, with any questions about the content of this site.

Copyright August 2009 – The Ohio State University. This material is based upon work supported by the National Science Foundation under Grant No. 0733024. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation. This work is licensed under an  Attribution-ShareAlike 3.0 Unported Creative Commons license .

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What does a melting glacier sound like? 'Gunshots.'

Glaciers are full of billions of loud bubbles—here’s what they tell us about our planet.

Tiny, pressurized air bubbles, trapped in ice, are accelerating the decline of some of the world’s glaciers, scientists have recently discovered.

In tidewater glaciers—large rivers of ice that pour into the sea—the steady melting of ice underwater causes billions of these bubbles to burst into the water “like little tiny gunshots,” says Erin Pettit, a glaciologist at Oregon State University in Corvallis, who is part of the team that made the discovery.

That violent pop of air stirs up the cold layer of water that hugs the surface of the glacial ice—bringing warmer water, several inches away, into contact with it. The bubbles then rise buoyantly through the water—driving turbulent currents that also bring warm water into contact with the ice.

The glaciers of Alaska, where Pettit’s team conducted the study, are currently losing over 70 billion tons of ice per year, a loss that causes seas to rise around the globe.

This new discovery stems from a 15-year effort by Pettit to understand an important but dangerous environment. In addition to improving our understanding of climate change, her efforts could also explain sharp reductions in the abundance of seals in some Alaskan fjords.

Unlocking the anatomy of a melting glacier

Few people realize it, but glaciers are full of tiny air bubbles. They form as snow, accumulating over thousands of years, slowly compresses into ice under its own weight—squishing the air that was trapped between snowflakes into microscopic pores. A cubic foot of glacial ice can hold over five million bubbles. Those bubbles are compressed to as much as 20 times the pressure of the Earth’s atmosphere.

Pettit and her colleagues had suspected for several years that these bubbles might cause the ice in tidewater glaciers to melt more quickly. To test this idea, they undertook a series of laboratory experiments.

They harvested blocks of bubble-rich ice from a tidewater glacier in Alaska called Xeitl Sít’ in Tlingit (also known as LeConte Glacier) and watched as the ice melted in a fish tank filled with sea water. As a comparison, they also melted blocks of bubble-free ice, which they purchased from a local ice sculpting artist.

As the ice melted, the resulting fresh water rose, because it was less dense than the surrounding sea water. This created a rising current along the vertical face of the ice—a microcosm of what occurs at the front of a real tidewater glacier. When the glacial ice melted, the current that it produced was six times faster than what was seen with the bubble-free ice because the rising bubbles pulled the water up more quickly. The glacial ice melted 2.25 times more quickly than the bubble-free ice.

“That’s a very powerful effect,” says Keith Nicholls, a polar oceanographer with the British Antarctic Survey in Cambridge, who was not part of the team. “If that’s the reality in nature, then it’s quite serious.”

The discovery was published today in the journal Nature Geoscience .

Discovering the “snap, crackle, and pop” of glaciers

Pettit’s first inklings that bubbles could be important came from monitoring glacier changes from afar.

Although huge amounts of melting happen at the calving fronts of tidewater glaciers, scientists are reticent to approach them too closely, due to the risks involved. The fronts of these glaciers tower up to 200 feet above the water, forming sheer walls that can send 50-ton ice blocks plunging downward at any moment, triggering waves that can crush or capsize small boats.

In 2009, Pettit tried to monitor the ice front from a safe distance in Icy Bay, Alaska, using hydrophones to record sounds underwater. She expected to hear icebergs calving off the glacier—perhaps even the low, garden-hose gurgle of a subglacial river gushing out from underneath the glacier.

But the main noise captured by these recordings was something more continuous, “like a sizzling pan of cooking food—a bit of snap, crackle, and pop,” says Pettit.

At 120 decibels, “the sounds were off the charts,” she says, louder than a car horn or a kitchen blender. The sounds were so loud that Jeffrey Nystuen, an oceanographer from the University of Washington who loaned her the hydrophones, believed the equipment was malfunctioning.

( Chile's glaciers are dying, and you can actually hear it—read more. )

Only after several more years of capturing recordings in other fjords did Nystuen finally embrace Pettit’s interpretation: that the sounds came from air bubbles popping out of the ice as it melted.

How bubbles expose glaciers to warming oceans

When Pettit published those observations back in 2015, she hoped to use the underwater sounds to monitor the rate of melting, and how it changed over the seasons. The full importance of the bubbles didn’t emerge until 2018, when she happened to discuss them with a newly hired professor at Oregon State.

As Pettit chatted over wine with Meagan Wengrove, an engineer and the study’s lead author, who studies the turbulence of rivers, they realized that those bubbles might actually mix up the thin ‘boundary layer’ of cold water that often insulates glacial ice from warm water. That very afternoon they rushed to out to a pet store and bought an aquarium that they would use in their newly published experiments.

Jonathan Nash, an oceanographer at Oregon State who is part of the team (and also Pettit’s husband), thinks that the bubbles probably exert their strongest melting effects in glaciers that thin substantially as they flow into the ocean, in places like Alaska, Canada, and Greenland—bringing ice that had been deeply buried up close to the surface.

These conditions will bring highly pressurized bubbles into the shallow part of the ocean (say the upper 300 feet) where the pressure inside the bubble is much higher than the surrounding water pressure—allowing the bubble to expand explosively and rise quickly.

Nash doesn’t expect these bubbles to have as much widespread impact in Antarctica, where most of the melting currently happens at far deeper depths, where the water pressure is higher—blunting the bubbles’ explosive effects.

What do bursting bubbles mean for rising seas?

These new results don’t mean that tidewater glaciers will melt and retreat twice as quickly as scientists had expected. But the new findings could help solve a long-standing mystery: in some tidewater glaciers in places like Alaska, Canada, and Greenland, the ice front is melting 10 times more quickly than scientists think it should, based on the water temperature.

The newly discovered bubble effect could explain some of that extra melting, says Mathieu Morlighem, a glaciologist at Dartmouth College in Hanover, New Hampshire. “It’s improving our understanding, but it’s not painting a darker picture of what’s happening today,” he says.

The new discovery will help scientists like Morlighem improve their models to better predict the future shrinkage of glaciers as oceans warm in the coming century. “It’s really, really critical,” he says. “We need a lot more work like this, to better understand the interaction between ocean water and the ice, and what drives that melt rate.”

New theories about bubbles in icy ecosystems

Pettit speculates that these glacial bubbles may have yet other, unseen effects in places like Alaska—perhaps even shaping aquatic ecosystems.

She notes that in Alaska, many fjords with tidewater glaciers have large populations of harbor seals. The animals shelter there while molting and raising pups. But in Glacier Bay, where the tidewater glaciers retreated many miles inland, the seal populations have declined. ­­­­

Pettit now suspects that the roaring patter of exploding bubbles provides a hiding place where seals can avoid detection by hungry orcas, which often find their prey by listening. The bubbles may mask the seals’ sounds—at least until the ice retreats out of earshot.

This may turn out to be yet another way in which these tiny bubbles have surprisingly large-scale effects—the proverbial ‘butterfly effect’—whereby tiny flapping wings spawn storms in distant places.

“Can these sub-millimeter bubbles actually affect the global ocean circulation” and global sea level? asks Nash: “Maybe they can.”

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The 50th Anniversary of the EROS Center: Honoring Five Decades of Innovation Through STEM Outreach Activities

  • September 7, 2023

By Ellie Leydsman McGinty

A Prominent Center for Earth Observation

The Earth Resources Observation and Science (EROS) Center recently celebrated its 50th anniversary from August 17-19, 2023. The EROS Center, located northeast of Sioux Falls, South Dakota, is a federal science center operated by the U.S. Geological Survey (USGS) that was established as a central repository for Landsat (formerly Earth Resources Technology Satellite) imagery, NASA aircraft and spacecraft data, and USGS aerial photography. Throughout its five decades of service, the EROS Center has become the primary steward of remotely sensed land images of the Earth, a pivotal leader in studying the Earth’s land areas and natural resources, and an authoritative provider of land change science data and information.  The inception of the EROS Center can be traced back to September 21, 1966, when Stewart Udall, then-Secretary of the Interior, issued a press release announcing Project EROS: An Earth Resources Observation Satellite Program. Project EROS was visualized as a collaborative USGS-NASA interagency Earth-observing satellite program that would acquire space-based data for natural and human resource management. After NASA signed the project approval document for the first Earth Resources Technology Satellite (ERTS-1) in January 1969, the USGS recognized the need for a facility that would process, distribute, and archive the data from the mission. Funds were accordingly appropriated in 1970 to build a data center. On March 31, 1970, a site near Sioux Falls, South Dakota, was strategically chosen based on data transmission investigations, socioeconomic needs, and political support. South Dakota Senator Karl E. Mundt was a key factor in generating the financial resources to make the data center possible. On August 7, 1973, the Karl E. Mundt Federal Building at the EROS Center was dedicated, and on January 1, 1974, the facility became fully operational. By the time the building was dedicated, ERTS-1 (later renamed Landsat 1) had been generating images for over one year. Employees of the EROS Center, who had been working in interim facilities in Sioux Falls, had already processed and produced an average of 25,000 images and photographs per month in response to requests from users all over the world. Within a year of the EROS Center becoming fully operational, imagery, photography, and electronic data from 16 different organizations were being distributed and archived.

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A Landmark Celebration

To commemorate the milestone anniversary of the EROS Center, a three-day celebration was held to honor 50 years of excellence and service to the local community, the nation, and the world. The celebration featured an evening community reception, a ribbon-cutting ceremony, a rededication event, and a “Friends and Family” open house. The open house consisted of special tours, science talks, alumni presentations, and STEM activities. AmericaView , a nationwide network of educators, took the lead in organizing and hosting a STEM event designed to engage learners across all age groups.  In collaboration with key partners, such as the NASA Landsat Communications and Public Engagement (CPE) Team, the NASA AREN AEROKATS Team, South Dakota State University, and South DakotaView , AmericaView curated several interactive stations for attendees in the USGS EROS Library that provided an overview of remote sensing and underscored the significance of Earth observation. The stations included the following offerings: a table with Landsat outreach materials; a Landsat collage activity; a Frustrationless Flyer kite -building and coloring activity; thermal (FLIR) camera and drone displays; and a demonstration of the STELLA handheld spectrometer . The STEM event had high levels of attendance and engagement, with visitors enjoying hands-on activities and eager to learn more about the Landsat Program and Earth observation.

Photos of the STEM event at the EROS Center 50th anniversary celebration.

A Spotlight on STELLA

During the event, the STELLA handheld spectrometer became a focal point of interest. STELLA (Science and Technology Education for Land/Life Assessment), a portable do-it-yourself (DIY) scientific instrument developed by the Landsat CPE Team, supports remote sensing education and outreach through scientific inquiry and discovery. As a DIY build, students, teachers, and young scientists can gain hands-on experience in science, technology, and engineering as they follow freely available online plans, instructions, and activities. With state-of-the-art sensors, STELLA measures the intensity of light reflected from surfaces across 12 different wavelength ranges in the visible and near-infrared regions of the electromagnetic spectrum. The instrument also encompasses sensors that measure surface temperature (emitted far infrared light). The spectral measurements acquired by STELLA correspond to those collected by sensors on Landsat satellites.  Attendees of the EROS 50th anniversary STEM event were drawn to the educational value and versatility of STELLA. The device offers a wide range of STEM-based learning activities, from building and programming an instrument to collecting, visualizing, and interpreting real-world scientific data. Guests were inspired by the capabilities and potential applications of the device, as the demonstration provided a foundational understanding of how the sensors on Landsat satellites collect data and how the data can be used to assess vegetation health. The online STELLA Dataviewer provided a platform for displaying, understanding, and exploring the spectral responses from different surfaces and materials. The STELLA augmented reality (AR) promotional card, which allows viewing of a 3D STELLA model on Instagram, served as a fascinating conversation piece and interactive experience.

Screenshot image of the STELLA Dataviewer webpage.

Related Reading

+ USGS EROS Celebrates 50 Years of a Mission that Matters

+ Celebrating a Half-Century at EROS: Serving the Nation and the World Since 1973

+ EROS History Timeline

+ AmericaView Supports USGS EROS in Celebrating 50 Years of Science and Discovery

+ STELLA: A DIY Handheld Scientific Instrument

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COMMENTS

  1. NASA: Earth's warming climate shrink glaciers by 50 percent

    The model aimed to predict the outcome of melting glaciers if Earth's temperatures increased by 1.5 to 4 degrees Celsius (about 2.7 to 5 degrees Fahrenheit) compared to pre-industrial levels.

  2. Glacier Worksheet Teaching Resources

    There are three versions of this worksheet .Included:Fill in the Blank Version with Key (includes optional word bank)Circle the Correct Answer Version with keyNote-talking Version (true, scientific information vs made-up information like the bus shrinking)The different versions coul Subjects: Earth Sciences, Other (Science), Science Grades:

  3. PDF GLACIERS: MOVERS AND SHAPERS I. A Tour in the Life of a Glacier

    Glaciers Worksheet 1 Earth Science Name: Surface Processes & Landscape Development Section: GLACIERS: MOVERS AND SHAPERS Directions: Using the Earth Science textbook pages 318 - 328 or use the web site: http://nsidc.org/glaciers/story/ answer the following questions. I. A Tour in the Life of a Glacier 1.

  4. Half of Earth's glaciers could vanish with 1.5 degrees of warming

    The study found that with 1.5 degrees Celsius of warming, 50% of the world's glaciers would disappear and contribute 9 centimeters (3.5 inches) to sea level rise by 2100. If the world reaches 2.7 ...

  5. Glacier Facts & Worksheets for Kids

    Glacier Worksheets Download includes the following worksheets: Frequently Asked Questions What is a glacier? How does a glacier get its name? How does glacier forms? Why is glacier ice blue? How does climate change affect glaciers? A glacier is an enduring body of thick ice that moves under its weight.

  6. Glaciers

    WORKSHEETS Science and Social Studies: Glaciers - Good and Bad Effects Distribute a reading selection and critical thinking questions about the effects of glaciers on land formation. Subjects: Science Geologic Formations

  7. Earth Science Glaciers Worksheets

    More complicated field of earth science glaciers worksheets have occurred. This pressure turns the lower parts of the so into ice. An Overview of Interactions and Feedbacks Between Wiley. Above which of worksheets that reduces friction is sedimentary prism, earth science worksheets that. Pfeffer locks onto the target and shoots a laser that ...

  8. Free Printable Earth Science Worksheets

    Free Printable Earth Science Worksheets. Investigate the planet Earth with these assessments on its structure, processes, and resources. Earth Science activities include rock classification and diagramming the rock cycle. Worksheets labeled with are accessible to Pro subscribers only. Become a Subscriber to access hundreds of premium worksheets.

  9. Earth Scientist Studying Glaciers

    EGO am an Earth Scientist who studies glaciers the ice sheets. MYSELF focus on how particles from land and who atmosphere end up in the ice and impact ice melt. Tell used an little pitch about your job. ME study how glaciers and ice sheets replace over time. To do this, I use satellite data and information collected from actual glaciers and ice ...

  10. Evidence found in Himalayas reveals half of Earth's glaciers will

    In a groundbreaking study led by Dr. David Rounce, assistant professor at Carnegie Mellon University, it has been estimated that the world's glaciers could lose as much as 40% of their mass by 2100 due to global warming. The research, published in the journal Science, is based on extensive fieldwork conducted by Rounce and his team from 2013 to ...

  11. Ice Age

    Color the ice (glaciers) gray. Color the water blue. Color the land green. Click here to print this worksheet.

  12. Glacier Worksheets

    Worksheets are Work glaciers, Glaciers practice questions and answers revised november, The melting glaciers, Katla geopark an educators guide and work, Im melting im melting, Glacier then now, Katla geopark an educators guide and work, Work extreme earth. *Click on Open button to open and print to worksheet.

  13. Worksheet

    This worksheet has 31 Earth Science Regents questions about the effect of glaciers on the landscape of New York State. There are both multiple choice and short answer questions.

  14. Glaciers Worksheet Teaching Resources

    $5 - $10 $10 and up Results for glaciers worksheet 1,352 results Sort: Relevance View: Sea Ice Glaciers and Sea Level Rise Article and Worksheet Climate Change Reading by Flying Colors Science

  15. Whittaker, Kathryn

    Regents Earth Science-Copies of Course Expectations, Worksheets, Labs and Honors Projects; Periods 1/4/8 Regents Earth: Distance Learning March 16- ... Glaciers. Oceans and Coastal Processes . Landscapes. Measuring Landscape Characteristics . METEOROLOGY. Energy and Seasons.

  16. Glaciers: Moving Rivers of Ice / Ice Sheet

    A glacier is a huge mass of ice that movement slowly over land. The term "glacier" comes from and Gallic word glace (glah-SAY), which means ice.Glaciers are often called " rivers of ice." Glaciers drop into two groups: alpine glaciers and ice sheets. Alps glaucers form on mountainsides and drive downward through valleys.Sometimes, alpine glaciers create or deepen valleys by pushing dust,

  17. Glaciers

    44 Q&A More from Geo-Earth Sciences Description Glaciers - Introduction and Types Activity to introduce or review Glacier information. Page 1 - Introduction to general Glacier information with Vocabulary and Word Bank fill in paragraph. Page 2 - Alpine Glaciers: Vocabulary, Reading and "Fill-Ins" Page 3 -

  18. How Do Glaciers Cause Erosion?

    Enrich your study of Earth science with this worksheet about glaciers and erosion. In this printable, students will circle the term that makes each statement true. As a skill challenge, they will analyze diagrams of two valleys and explain the role of a glacier in their formation. Grade: 6 | 7 | 8 | 9 Subjects: Science Earth Science Glaciers

  19. Unraveling a paradox of Himalayan glacier melt

    One in five glaciers on Earth are covered with a layer of rocky debris. The presence of debris influences how glaciers melt. In the Himalaya, debris covers most large glaciers, and it is so thick ...

  20. Glaciers Worksheet

    This free printable worksheet all about Glaciers for kids has a fun word seek game along with a find-the-hidden-and-missing words puzzle. This science kids words game is free to download and print at no cost. Our fun facts on Glaciers worksheet is enjoyable for kids in Grammar school in 1st Grade to 5th Grade as well as for younger kids in ...

  21. Hands-on Lessons and Activities about Glaciers

    (Grades K-5) Students model the formation of ice with marshmallows or, if it is available, snow. Lesson extensions suggest using snow cones or shaved ice to model the difference between snow, firn (an intermediate stage between snow and ice), and glacial ice.

  22. earth science glaciers worksheets

    A Tour in the Life of a Glacier 1. Mar 5, 2015 - This worksheet has 20 Earth Science Regents questions about the effect of glaciers on landscapes. Great mix of reading and math. Glacier Worksheets. Glaciers Worksheet 1 Earth Science Name: Surface Processes & Landscape Development Section: GLACIERS: MOVERS AND SHAPERS Directions: Using the Earth Science textbook pages 318 - 328 or use the web ...

  23. Glaciers: Ice That Flows Printable (5th

    Worksheets Science Glaciers: Ice That Flows Glaciers: Ice That Flows Download Add to Favorites In this activity, students learn how glaciers are formed and how they move materials around Earth. They then experiment with water, rocks, and sediment to create model glaciers. Grade: 5 | 6 | 7 | 8 Subjects: Science Earth Science Glaciers + show tags

  24. What does a melting glacier sound like? 'Gunshots.'

    The glaciers of Alaska, where Pettit's team conducted the study, are currently losing over 70 billion tons of ice per year, a loss that causes seas to rise around the globe.

  25. Results for Glaciers

    Worksheets, Activities, Printables Also included in: Science Passages: Nonfiction Texts bundle $3.00 5.0 (49) PDF

  26. Glaciers Unit Study: science on ice!

    Science on Ice: Glaciers is a unique earth sciences unit for kids! Students will teach all about valley glaciers, ice hood & ice shelf, and post-glacial landscapes! Plus it includes tons of product at paleoclimatology, ice cores exploring, atmosphere change, glacial natural, and more! teilbereich 8.3 plains Flashcards ...

  27. Ice and Glaciers Worksheet / Worksheet, worksheet

    Ice and Glaciers Worksheet 4.7 (3 reviews) Geography Human and Physical Geography Geographical Features Free Account Includes: Thousands of FREE teaching resources to download Pick your own FREE resource every week with our newsletter Suggest a Resource! You want it? We'll make it 24/7 customer support (with real people!) Sign Up Now to Download

  28. The 50th Anniversary of the EROS Center: Honoring Five Decades of

    The Earth Resources Observation and Science (EROS) Center recently celebrated its 50th anniversary from August 17-19, 2023. The EROS Center, located northeast of Sioux Falls, South Dakota, is a federal science center operated by the U.S. Geological Survey (USGS) that was established as a central repository for Landsat (formerly Earth Resources Technology Satellite) imagery, NASA aircraft and ...