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関連する概念動画

Bone Remodeling01:40

Bone Remodeling

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Bone remodeling is a continuous and balanced process of bone resorption by osteoclasts and bone formation by osteoblasts. In adults, it helps maintain bone mass and calcium homeostasis. While mechanical stress can stimulate turnover as part of the normal maintenance and reparative process, several hormones also regulate bone remodeling.
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Global Climate Change01:50

Global Climate Change

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Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
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Osteoclasts in Bone Remodeling01:31

Osteoclasts in Bone Remodeling

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Osteoclasts are cells responsible for bone resorption and remodeling. They originate from hematopoietic progenitor cells present in the bone marrow. Numerous progenitor cells fuse to form multinucleated cells, each with 10-20 nuclei. A single osteoclast has a diameter of 150 to 200 µM. These cells have ruffled borders that break down the underlying bone tissue and release minerals such as calcium into the blood in bone resorption. Osteoclasts cling to bones with their ruffled edges during...
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Quarrying of Stone01:15

Quarrying of Stone

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Quarrying is the process of extracting stone from a quarry, where specialized techniques are employed to remove large blocks of stone safely and efficiently. This process can involve controlled explosions or more precision-oriented methods such as cutting and drilling.
One common method involves using a diamond belt saw to cut large blocks from the quarry face. These blocks can be about 50 feet long and 12 feet high. After the initial vertical cut, drilling is performed at the base of the...
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Frost Action on Concrete01:27

Frost Action on Concrete

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Concrete structures in cold climates, such as those along roadsides, can retain moisture. This moisture makes them susceptible to frost-related damage when temperatures fall below freezing. Adding moisture worsens the damage during temperature fluctuations, leading to repeated freezing and thawing. De-icing salts, spread over these structures to melt ice, add to the freeze-thaw cycle, and draw even more moisture into the concrete.
This freeze-thaw cycle primarily causes surface scaling, where...
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Manipulation and Analysis01:21

Manipulation and Analysis

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GIS manipulation and analysis functions are vital for decision-making and planning. These activities range from data retrieval tasks, such as selecting information based on specific criteria, to advanced analytical techniques that address complex spatial problems.One critical GIS analysis method is overlaying, which combines multiple data layers to examine impacts. For example, overlaying a river-dammed lake boundary with road networks can identify affected infrastructure. Another common...
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関連する実験動画

Updated: May 6, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

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氷河は,山岳の形成に対する破壊的および建設的なコントロールとして,氷河を形成します.

Stuart N Thomson1, Mark T Brandon, Jonathan H Tomkin

  • 1Department of Geosciences, University of Arizona, Tucson, Arizona 85271, USA. thomson@email.arizona.edu

Nature
|September 17, 2010
PubMed
まとめ

紀元後期の世界的な冷却はパタゴニアアンデスにおける侵食を加速し,氷河が山の侵食率を制御した. 最南端のアンデス山脈は,氷河の保護を示し,建設的な山の成長につながります.

科学分野:

  • 地質学 地質学 地質学
  • ジオモルフォロジー ジオモルフォロジー
  • 気候科学 気候科学

背景:

  • 理論的なモデルは,地球温暖化と侵食が山の形成の動態に影響を及ぼすことを示唆している.
  • アルプス山脈の氷河の侵食により,オロゲンの幅と高さが著しく減少すると予測されています.
  • 気候の冷却に対する地質学的反応に関するフィールド・エビデンスは,希少である.

研究 の 目的:

  • パタゴニアアンデス山脈におけるケノゾイク期後半の気候の冷却の影響を調査する.
  • 気候に起因する侵食に対する地質学的反応の現場証拠を集めること.
  • 氷河化,侵食,山岳形成の関係を理解する.

主な方法:

  • パタゴニアアンデス (38°Sから56°S) の低温熱クロノロジーデータ収集.
  • 侵食の歴史を再構築するために冷却時代の分析.
  • 侵食パターンが,氷河の歴史と地質学的な活動と相関している.

主要な成果:

  • 侵食率の大幅な増加は700万~500万年前に発生し,パタゴニア氷河期と一致した.
  • 最も高い侵食率は,氷河平衡線の高さにある風向きの側面で観察されました.

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関連する実験動画

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Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
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  • 侵食の減少とオロゲンの高さの増加は,より高い緯度 (49°S-56°S) で観察されました.
  • 結論:

    • パタゴニアアンデス山脈は,気候変動による侵食が山の形成に影響を与えているという最初のフィールド証拠を提供します.
    • 氷河の侵食率は,氷河の平衡線の高さと氷の滑り速度と密接に関連しています.
    • 南極アンデスにおける地域の氷河保護は,他の場所での侵食による減少と対照的に,建設的な成長をもたらした.