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Glaciers Are Alive
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Hotel Des Glaciers
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Glaciers, 1870 Painting 35x30
Glaciers, 1870 Painting, prepared on 100% cotton canvas, is specially prepared for you upon your order. Our paintings, coated with special odorless satin varnish, are easy to clean and retain their first-day liveliness for many years. Product Code: AIK 070 100% Cotton Lined Canvas (Canvas) Stretching on Wooden Chassis with 3 cm Edge Thickness Special Satin Varnish Coating and Easy Cleaning Hand Workmanship High Definition Print Quality Shock Resistant Special Packaging We Guarantee Satisfaction on Every Canvas Painting We Produce Listed By ENTEGRA
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Building Rural Community Resilience Through Innovation and Entrepreneurship
Drawing from empirical analyses, case studies, and a synthesis of best practices, this book explores how innovation manifests itself in rural places and how it contributes to entrepreneurial development and resilience.Innovation in rural places may come about as a result of new forms of collaboration; policies that leverage rural assets and address critical service or product gaps; novel strategies for accessing financial capital; infusion of arts into aspects of community life; and cultivation of networks that bridge entrepreneurs, organizations, and institutions.The chapters illustrate how a number of innovation-related characteristics relate to economic vibrancy in rural places such as a strong connection to the arts, adaptive and sustainable use of natural resources, value-chain integrated food systems, robust bridging social capital networks, creative leveraging of technology, and presence of innovation-focused entrepreneurs.Through exploration of these and other topics, this book will provide insights and best practices for rural community and economic development scholars and practitioners seeking to strengthen the rural innovation ecosystem.
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How do glaciers melt?
Glaciers melt primarily due to a combination of rising temperatures and the effects of sunlight. When the air temperature increases, the heat is transferred to the glacier, causing the ice to melt. Additionally, sunlight can also contribute to the melting process by absorbing heat and accelerating the melting of the ice. As the ice melts, the water flows into rivers and oceans, contributing to rising sea levels. This process is exacerbated by climate change, which is causing glaciers to melt at an accelerated rate.
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How can glaciers shape rocks?
Glaciers can shape rocks through a process called glacial erosion. As glaciers move, they pick up rocks and debris, which act as tools to grind and scrape the underlying bedrock. This process can create features such as striations, grooves, and polished surfaces on rocks. Additionally, as glaciers melt, they can deposit the rocks they were carrying, forming landforms like moraines and drumlins.
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How can glaciers erode rocks?
Glaciers can erode rocks through a process called plucking and abrasion. Plucking occurs when the glacier freezes onto the rock and then pulls it away as the glacier moves, causing pieces of the rock to be plucked off. Abrasion occurs as the glacier moves and the rocks embedded in the ice scrape against the bedrock, wearing it down over time. These processes can result in the formation of glacial valleys, cirques, and other landforms as the glacier erodes the surrounding rock.
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What functions do glaciers have?
Glaciers play several important functions in the environment. They act as reservoirs of freshwater, storing large amounts of water in the form of ice. Glaciers also help regulate global climate by reflecting sunlight and cooling the Earth's surface. Additionally, they shape the landscape through processes like erosion and deposition, creating unique landforms such as valleys, fjords, and moraines. Overall, glaciers are crucial components of the Earth's system and have a significant impact on both the environment and human societies.
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Glaciers and Glaciation, 2nd edition
Glaciers and Glaciation is the classic textbook for all students of glaciation.Stimulating and accessible, it has established a reputation as a comprehensive and essential resource. In this new edition, the text, references and illustrations have been thoroughly updated to give today's reader an up-to-the minute overview of the nature, origin and behaviour of glaciers and the geological and geomorphological evidence for their past history on earth. The first part of the book investigates the processes involved in forming glacier ice, the nature of glacier-climate relationships, the mechanisms of glacier flow and the interactions of glaciers with other natural systems such as rivers, lakes and oceans. In the second part, the emphasis moves to landforms and sediment, the interpretation of the earth's glacial legacy and the reconstruction of glacial depositional environments and palaeoglaciology.
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Wilhelmina Barns-Graham : The Glaciers
In May 1949, the Scottish artist Wilhelmina Barns-Graham (1912-2004) visited the Grindelwald Glacier in Switzerland.It was a trip which would have a profound and lasting impact on her work.Charting the journey, the beautiful work it stimulated and wider questions around glacial landscapes, then and now, this publication provides insights that will expand our understanding of both an acclaimed body of work and the artist who created it. That Barns-Graham produced her final glacier painting in 1994, some 45 years after her sole visit to Switzerland, is testament to the influence that the experience had on her.So too are her 100 or so individual glacier works - made first between 1949 and 1952 and then in revisiting the subject between 1976 and 1994.Including a complete catalogue of the glacier paintings, this book presents the definitive account of a trip that would transform the artistic imagination of one of the foremost British painters of the twentieth century.
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Meltdown : The Earth Without Glaciers
We hear about pieces of ice the size of continents breaking off of Antarctica, rapidly melting glaciers in the Himalayas, and ice sheets in the Arctic crumbling to the sea, but does it really matter?Will melting glaciers change our lives? Absolutely. Glaciers are built and destroyed during ice ages and interglacial periods.These massive ice bodies hold three quarters of our freshwater, yet we don't have laws to protect them from climate change.When they melt, they increase sea levels, alter the Earth's reflectivity, wreak havoc for ocean and air currents, destabilize global ecosystems, warm our climate, and bring on floods that swamp millions of acres of coastal land.The critical ecological role they play to keep our global climate stable, and the environmental functions they provide, wither. And, as climate change warms glacier cores, collapsing glacier ice triggers tsunamis that send deadly massive ice blocks, rocks, earth, and billions of liters of water rushing down mountain valleys.It has happened before in the Himalayas, the Central Andes, the Rockies and Western Cascades, and the European Alps, and it will happen again. In his new book Meltdown, Jorge Daniel Taillant takes readers deeper into the cryosphere, connecting the dots between climate change, glacier melt, and the impacts that receding glacier ice brings to livability on Earth, to our environments, and to our communities.Taillant walks us through the little-known realm of the periglacial environment, a world of invisible subsurface rock glaciers that will outlive exposed glaciers as climate change destroys surface ice.He also looks at actions that can help stop climate change and save glaciers, exploring how society, politics, and our leaders have responded to address the global COVID-19 pandemic and yet largely continue to fail to address the even larger—looming and escalating—crisis of climate change. Our climate is deteriorating at a drastic rate, and it's happening right in front of us.Meltdown is about glaciers and their unfolding demise during one of the most critical moments of our planet's geological history.If we can reconsider glaciers in a whole new light and understand the critical role they play in our own sustainability, we may be able to save the cryosphere.
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Everyday Life-Environmentalism : Community Sustainability and Resilience in Asia
This book provides one of the first systematic introductions to the Japanese concept of life-environmentalism, Seikatsu-Kankyo Shugi.This concept emerged in the 1980s as a shared research framework among Japanese social scientists studying the adverse consequences of postwar industrialization on everyday life in communities. Life-environmentalism offers a lens through which the agency of small communities in sustaining their everyday life and living environment can be understood.The book provides an overview of this approach, including intellectual backgrounds and foundational concepts, along with a variety of empirical case studies that examine environmental and sustainability issues in Japan and other parts of Asia.It also includes critical reflections on the approach in light of contemporary sustainability challenges.The empirical topics covered in the book include local community responses to development projects, resource governance, disaster response and recovery, and historical environmental preservation.The chapters are contributed by researchers working at the forefront of the field.It provides only a glimpse into the vast literature that awaits further exploration and engagement in the future. The book is suitable for upper undergraduate students, graduate students, and researchers interested in environmental problems, sustainability and resilience, disaster mitigation and response, and regional development in Asian contexts, particularly Japan.It is well-suited for courses in anthropology, geography, sociology, urban and regional planning, political science, Asian studies, and environmental studies.
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Why are glaciers the Earth's thermometers?
Glaciers are considered the Earth's thermometers because they are sensitive indicators of climate change. As temperatures rise, glaciers melt at a faster rate, and their size and extent decrease. By studying the changes in glaciers, scientists can track variations in temperature over time. Additionally, the composition of the ice in glaciers can provide information about past climate conditions, making them valuable tools for understanding the Earth's climate history.
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Under what conditions do glaciers form?
Glaciers form under specific conditions of temperature and precipitation. They require cold temperatures to prevent the snow from melting, and a consistent accumulation of snowfall over time. This snow then compresses into ice, forming a glacier. Glaciers are typically found in polar regions or high mountainous areas where these conditions are met.
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What are the different types of glaciers?
There are two main types of glaciers: alpine glaciers and ice sheets. Alpine glaciers are found in mountainous regions and flow down valleys, while ice sheets are massive glaciers that cover large areas of land. Other types of glaciers include tidewater glaciers, which flow into the ocean, and hanging glaciers, which are perched on steep slopes. Each type of glacier has unique characteristics and plays a crucial role in shaping the landscape and influencing climate.
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How have glaciers shaped the ground cover?
Glaciers have significantly shaped the ground cover through processes like erosion, deposition, and transportation of sediments. As glaciers move, they scrape and erode the land, creating valleys, fjords, and cirques. The sediments carried by glaciers are deposited as moraines, drumlins, and eskers, altering the landscape. The melting of glaciers also contributes to the formation of lakes and wetlands, further shaping the ground cover.
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