Video Experimental Relacionado
Updated: Jul 6, 2026

09:06
Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside
Published on: July 3, 2016
Edades terrestres de cuatro meteoritos de Allan Hills: consecuencias para el hielo antártico
Resumen
Las edades terrestres de los meteoritos revelan que la capa de hielo de la Antártida tiene más de 1,54 millones de años. La recolección de meteoritos en Allan Hills probablemente comenzó hace entre 30.000 y 300.000 años.
Área de la Ciencia:
- Cosmoquímica y Ciencias Planetarias.
- Geocronología Geocronología.
- Glaciología glaciología.
Sus antecedentes:
- Comprender las edades terrestres de los meteoritos proporciona información sobre la historia ambiental de la Tierra.
- La región de Allan Hills en la Antártida es un sitio conocido para la recuperación de meteoritos.
- La datación de los meteoritos ayuda a establecer edades mínimas para la estabilidad de la capa de hielo.
Objetivo del estudio:
- Para determinar las edades terrestres de los meteoritos de Allan Hills.
- Para inferir la edad mínima de la capa de hielo de la Antártida.
- Para estimar el inicio de la acumulación de meteoritos en Allan Hills.
Principales métodos:
- Datación radiométrica de muestras de meteoritos.
- Análisis de núcleos cosmogénicos para determinar la duración de la exposición terrestre.
Principales resultados:
- Tres meteoritos de Allan Hills tienen edades terrestres entre 3 x 10^4 y 3 x 10^5 años.
- Un meteorito tiene una edad terrestre de (1.54 ± 0.14) x 10^6 años.
- La capa de hielo de la Antártida tiene más de 1,54 millones de años.
Conclusiones:
- La edad mínima de la capa de hielo antártica se establece en más de 1,54 millones de años.
- La acumulación de meteoritos en Allan Hills probablemente comenzó hace entre 3 x 10^4 y 3 x 10^5 años.
- Estos hallazgos contribuyen a reconstruir la historia glacial de la Antártida y los eventos de caída de meteoritos.
Videos de Conceptos Relacionados
What is Climate?
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Global Climate Change
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.
Conditions on Early Earth
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Conditions on Early Earth
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Cold Weather Concreting
When freshly poured concrete is exposed to freezing temperatures before it has set, the water within the concrete can freeze. This expansion disrupts the setting process, delays chemical reactions necessary for hardening, and increases the volume of pores within the hardened concrete, which weakens its overall structure. If the concrete manages to reach an appreciable strength before it freezes, the damage can be somewhat mitigated.
To counteract the negative impacts of cold weather, ensuring...
To counteract the negative impacts of cold weather, ensuring...
Frost Action on Concrete
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...
This freeze-thaw cycle primarily causes surface scaling, where...

