Question

География!7класс ( помогите пожалуйста). Кто первым ответит на все вопросы, тот ответ я провозглашу ЛУЧШИМ!! 1. Назовите оболочки Земли ,образующие географическую оболочку. 2. Какие круговороты существуют в географической оболочке 3. Какие свойства есть географической оболочки 4.Что называют широтный зональностью? 5. Определите черты сходства и различия между широтой зональностью выращенный на равнинах и высотой поясностью в горах. 6. Для чего любому человеку необходимы знания в географической оболочки её строении свойствах.

Answer 1

1.атмосфера,гидросфера, биосфер, литосфера.
2.теплые, холодные течения, круговороты воды.
3.Географической оболочка отличается очень большой сложностью состава и разнообразным состоянием вещества;В географической оболочке сосредоточена жизнь и существует человеческое общество;Все физико-географические процессы в этой оболочке протекают за счет солнечной и внутренней энергии Земли;Все виды энергии поступают вгеографическую оболочку, трансформируются в ней и частично консервируются.
4.закономерное изменение физико-географических процессов, компонентов и комплексов геосистем от экватора к полюсам.
5.СХОДСТВА: 
1. ПТК природных зон и высотных поясов формируются в силу определённого соотношения тепла и влаги: чем холоднее и чем меньше влаги, тем как правило, меньше продуктивность ПТК, меньше плодородие почв. 
2. Каждый высотный пояс имеет свой аналог среди равнинных природных зон. Так, поясу альпийских лугов на равнине соответствует зона лесотундры, а поясу лиственных лесов (например, в горах Кавказа) - соответствующая природная зона в центре Восточно-Европейской равнины. 
3. Широтные и высотные пояса сменяют друг друга в сходной последовательности: от экватора к полюсам и от подножья гор к вершине. Каждые 100 метров подъёма соответствуют 100 километрам в широтном направлении по равнине. Поднялись на 1 км - как будто поехали 1000 км на север (ну или на юг, если это, скажем, Анды) . 

РАЗЛИЧИЯ: 
1. Широтная зональность возникает на равнинах в силу уменьшения суммарной солнечной радиации, а высотная поясность - в горах по причине понижения температуры в тропосфере при подъёме. На каждый километр подъёма температура понижается на 6 градусов. 
2. Природные зоны гораздо больше по площади. Кроме того, высотные пояса часто представлены отдельными фрагментами, не образуя сплошного покрова территории.
6.мое мнение чтобы хорошо ориентироваться

Answer 2

Geographical Envelopes of the Earth

The Earth is composed of several layers or envelopes that form its geographical envelope. These envelopes include:

1. Lithosphere: The lithosphere is the solid outer layer of the Earth. It consists of the Earth's crust and the uppermost part of the mantle. The lithosphere is divided into several tectonic plates that float on the semi-fluid asthenosphere below.

2. Hydrosphere: The hydrosphere refers to all the water on Earth, including oceans, seas, lakes, rivers, groundwater, and even water vapor in the atmosphere. It covers about 71% of the Earth's surface.

3. Atmosphere: The atmosphere is the layer of gases that surrounds the Earth. It is composed of nitrogen (about 78%), oxygen (about 21%), and traces of other gases such as carbon dioxide, water vapor, and argon. The atmosphere plays a crucial role in regulating the Earth's climate and weather patterns.

4. Biosphere: The biosphere is the zone of life on Earth. It includes all living organisms, from microscopic bacteria to plants, animals, and humans. The biosphere interacts with the other envelopes and is responsible for the diversity of life on our planet.

Circulation Patterns in the Geographical Envelope

The geographical envelope of the Earth exhibits various circulation patterns, which are important for understanding the Earth's systems. Some of these circulation patterns include:

1. Oceanic Circulation: Ocean currents are large-scale movements of water in the oceans. They are driven by a combination of factors, including wind, temperature, salinity, and the Earth's rotation. Ocean currents play a crucial role in distributing heat around the globe, influencing climate patterns, and affecting marine ecosystems.

2. Atmospheric Circulation: Atmospheric circulation refers to the movement of air in the Earth's atmosphere. It is driven by the unequal heating of the Earth's surface by the sun. This circulation pattern creates global wind systems, such as the trade winds, prevailing westerlies, and polar easterlies. Atmospheric circulation is responsible for weather patterns and the distribution of heat and moisture around the globe.

3. Water Cycle: The water cycle, also known as the hydrological cycle, is the continuous movement of water on, above, and below the Earth's surface. It involves processes such as evaporation, condensation, precipitation, and runoff. The water cycle is essential for maintaining the availability of freshwater and regulating the Earth's climate.

Properties of the Geographical Envelope

The geographical envelope of the Earth possesses several properties that are important to understand. These properties include:

1. Interconnectedness: The different envelopes of the Earth are interconnected and influence each other. Changes in one envelope can have cascading effects on the others. For example, changes in ocean temperatures can impact atmospheric circulation patterns and weather systems.

2. Dynamic Nature: The geographical envelope is constantly changing and evolving. Earthquakes, volcanic eruptions, erosion, and weathering shape the Earth's surface. Climate patterns and ecosystems also undergo changes over time.

3. Spatial Variation: The properties and characteristics of the geographical envelope vary from one location to another. Factors such as latitude, altitude, proximity to water bodies, and geological features contribute to this spatial variation.

Latitudinal Zonation and Altitudinal Zonation

4. Latitudinal Zonation: Latitudinal zonation refers to the division of the Earth's surface into distinct climatic zones based on latitude. As one moves from the equator towards the poles, there are noticeable changes in temperature, precipitation, vegetation, and animal life. This zonation is influenced by factors such as solar radiation, atmospheric circulation, and the Earth's tilt.

5. Altitudinal Zonation: Altitudinal zonation, on the other hand, refers to the division of the Earth's surface into distinct zones based on altitude or elevation. As one ascends a mountain or a highland, there are changes in temperature, precipitation, vegetation, and animal life. This zonation is influenced by factors such as temperature lapse rate, air pressure, and the availability of moisture.

While both latitudinal zonation and altitudinal zonation involve the division of the Earth's surface into zones based on certain characteristics, there are some similarities and differences between them:

- Similarities: Both zonation patterns involve changes in temperature, precipitation, vegetation, and animal life. They are influenced by factors such as solar radiation, temperature lapse rate, and the availability of moisture.

- Differences: Latitudinal zonation is primarily influenced by latitude and the angle of solar radiation, while altitudinal zonation is influenced by changes in altitude or elevation. Latitudinal zonation is more gradual and spans larger areas, while altitudinal zonation can change rapidly over shorter distances.

Importance of Understanding the Geographical Envelope

Knowledge about the geographical envelope and its properties is essential for several reasons:

1. Understanding the Earth's Systems: The geographical envelope is the foundation for studying various Earth systems, including climate, weather, ecosystems, and natural resources. Understanding these systems helps us comprehend the complex interactions between the Earth's spheres and how they shape our planet.

2. Environmental Awareness: Knowledge about the geographical envelope enables us to understand the impact of human activities on the Earth's systems. It helps us recognize the importance of sustainable practices and the need to protect and conserve our natural resources.

3. Spatial Analysis: Understanding the properties and characteristics of the geographical envelope allows us to analyze spatial patterns and make informed decisions related to land use, urban planning, agriculture, and resource management.

4. Cultural and Historical Significance: The geographical envelope has played a significant role in shaping human civilizations throughout history. It has influenced settlement patterns, trade routes, cultural practices, and the distribution of resources.

In conclusion, the geographical envelope of the Earth consists of the lithosphere, hydrosphere, atmosphere, and biosphere. It exhibits various circulation patterns and possesses properties such as interconnectedness, dynamic nature, and spatial variation. Latitudinal and altitudinal zonation are important concepts in understanding the Earth's climatic patterns. Knowledge about the geographical envelope is crucial for understanding Earth systems, environmental awareness, spatial analysis, and recognizing the cultural and historical significance of our planet.