What are the positive impact that buffering will have on the environmental sustainability

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Answer 1

Preservation of riparian supports can emphatically affect agribusiness by diminishing disintegration, further developing water quality, expanding biodiversity, and extending natural life living spaces.

Supports eliminating residue from surface spillover and diminishes centralizations of supplements and pesticides.

By carrying out transforms, you will have a more modest carbon impression and diminish the number of poisons delivered into the environment. People in the future eventually benefit from further developed air and water quality, fewer landfills, and more environmentally friendly power sources.

Streamside cushions are a significant piece of stream biological systems since they decline contamination, control disintegration, and give untamed life natural surroundings. Additionally called riparian supports, streamside cushions are normally happening in vegetated regions that run close by streams and other amphibian frameworks like lakes, lakes, and wetlands.

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which of the following are geologic settings where travertine can form? choose one or more: a. in glacial lakes b. in caves c. in fast-moving rivers d. near hot springs e. in swamps

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Travertine can form in a variety of geologic settings, including in caves,  near hot springs, and  in fast-moving rivers. Therefore the correct option is option A, B and C.

In caves, travertine forms as a result of carbon dioxide in the air dissolving in water. This results in an increase in the acidity of the water, which in turn dissolves the rock the cave is made of and deposits the resulting sediment in the form of travertine.
Near hot springs, the water is saturated with dissolved minerals such as calcium carbonate, which can also be deposited in the form of travertine.
In fast-moving rivers, the increased turbulence can cause the suspended sediment in the water to become trapped and deposited in the form of travertine.
Travertine can also form in glacial lakes, but not in swamps.

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which element is found in greater amounts in low viscosity magma, than in high viscosity magma? question 12 options: a) si b) fe

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Si (Silica) is found in greater amounts in low viscosity magma, than in high viscosity magma. Option A is correct answer.

High silica content magmas will consequently show higher levels of polymerization and have higher viscosities than magmas with low silica concentration. A substance's viscosity is a measurement of its consistency. A substance's viscosity is defined as its capacity to resist flow. Viscosity is, in some ways, the inverse of fluidity. Because cold molasses is less fluid than water, it has a greater viscosity.

The temperature, composition, and gas concentration of a magma all influence its viscosity. The relationship between temperature and viscosity is self-evident. The greater the temperature, like with most liquids, the more fluid the material becomes, reducing its viscosity.

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based upon your analysis, most stratovolcanoes form in which tectonic setting? group of answer choices divergent boundaries oceanic-continental convergent boundaries mantle plumes (hotspots) all of the above

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The correct option is All of the above i.e. D. Most stratovolcanoes form in convergent boundaries, which occur when two tectonic plates collide. This collision causes one of the plates to slide beneath the other, creating a subduction zone.

The subducting plate melts due to the extreme pressure and heat created from the collision, resulting in magma being forced upward to form a stratovolcano. Oceanic-continental divergent boundaries can also form stratovolcanoes, as the plate separation creates a rift zone.

Mantle plumes, also known as hotspots, can also form stratovolcanoes when a column of hot material from the mantle rises up through the Earth's crust, creating a weak area of the crust which can then be filled with magma. All of these tectonic settings can create stratovolcanoes. The correct option is All of the above i.e. D.

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What are the three ways In which corruption will negatively affect the financial growth of South Africa​

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Answer:

unemployment, reduction in tax revenue, decline in business operation and ultimately, collapse of the economy

he san andreas fault is... group of answer choices associated with deep focus earthquakes a world-famous example of a hot spot is an intraplate fault within the juan de fuca plate an oceanic transform fault a continental transform fault

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The San Andreas Fault is a continental transform fault, which is a type of fault that occurs at the boundary between two tectonic plates.

The San Andreas Fault marks the boundary between the Pacific Plate and the North American Plate. The two plates slide past each other horizontally in opposite directions. As the plates move, they cause earthquakes with deep focus, which are powerful earthquakes that occur far beneath the surface.

An example of a world-famous hot spot is the Hawaii Islands, which form due to magma rising up from the Earth's mantle. This is a form of intraplate volcanism, which occurs at locations that are not on tectonic plate boundaries. In contrast, transform faults are located on plate boundaries, and the San Andreas Fault is a prominent example.

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8. What is the collective role of water vapor, carbon dioxide, ozone, and methane in the atmosphere?

A. They prevent harmful ultraviolet radiation of the sun from reaching earth
B. they are important components of the water cycle, which regulates the earths temperature
C. they regulate earths climate by trapping heat and holding it within earths atmosphere
D. they scatter almost a third of the sunlight that reaches the outer layers of the atmosphere back into space ​

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Answer: C. They regulate Earth's climate by trapping heat and holding it within Earth's atmosphere. 

what is an aquifer, igneous and metamorphic rocks are not good aquifers as they contain little natural porosity or permeability.

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An aquifer is an underground layer of water-bearing permeable rock, rock fractures or unconsolidated materials (gravel, sand, or silt) from which groundwater can be extracted. Igneous and metamorphic rocks generally contain little natural porosity or permeability and therefore cannot be used as aquifers. Igneous rocks, for instance, form when molten magma cools and solidifies.

The cooling process does not leave much space for porosity and permeability. The recrystallization of the rock grains during metamorphism also does not leave much space for porosity and permeability.

Aquifers can be found in sedimentary rocks like sandstone, limestone and shale because the grains of these rocks are arranged in a way that allows for more porosity and permeability.

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What are the 5 stages of solar system formation?

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The 5 stages of solar system formation are Solar Nebula, Protostar and Protoplanetary Disk, Planetesimals, Protoplanets and  Solar System.

The 5 stages of solar system formation are:

1. Solar Nebula: A cloud of dust and gas, called the solar nebula, begins to collapse due to gravitational forces. As it collapses, the material starts to spin and flatten into a disk shape.

2. Protostar and Protoplanetary Disk: The material in the center of the disk becomes denser, forming a protostar. Meanwhile, the remaining material in the disk starts to clump together, creating a protoplanetary disk around the protostar.

3. Planetesimals: Within the protoplanetary disk, solid particles collide and stick together, forming larger bodies called planetesimals. These planetesimals continue to grow as they collect more material from the disk.

4. Protoplanets: As planetesimals grow and interact, some merge through collisions, eventually forming larger bodies known as protoplanets. Protoplanets continue to evolve and differentiate, developing into the planets we observe in our solar system today.

5. Solar System: Over time, the protostar at the center of the system becomes a fully-fledged star (our Sun), while the remaining protoplanetary disk material is cleared out, leaving the planets, moons, asteroids, and other bodies orbiting the star. This marks the formation of the solar system.

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despite having a lower global warming potential and a shorter residence time in earth's atmosphere, co2 is the most important radiative forcing behind global warming because -

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CO2 is the most important radiative forcing behind global warming because it is the most abundant of all the greenhouse gases in the atmosphere and its residence time in the atmosphere is very long.

This allows it to accumulate and persist over a long period of time, and so its radiative forcing effect is greater than other greenhouse gases with a lower global warming potential and a shorter residence time.

While other greenhouse gases, such as methane and nitrous oxide, have a greater warming potential, they are present in much smaller quantities in the atmosphere than CO2.

Furthermore, CO2 emissions have been increasing steadily due to human activities such as burning fossil fuels and deforestation, leading to a buildup of CO2 in the atmosphere over time

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the annual cycle of prevailing weather conditions at a given place based on long-term contitions is known as: weather. a trend cyclone climate global warming

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The annual cycle of prevailing weather conditions at a given place based on long-term conditions is known as climate.

The term weather is used to refer to short-term conditions such as precipitation, temperature, and wind. The climate of a region is determined by a variety of factors, including latitude, elevation, prevailing winds, and the presence of land and water bodies.

It can be classified into different categories based on temperature, precipitation, and other factors. In general, climate change refers to long-term changes in weather patterns and temperature around the world, while global warming refers specifically to the gradual warming of the planet's surface due to increased levels of greenhouse gases in the atmosphere. Cyclones, on the other hand, are severe tropical storms that can cause significant damage and loss of life. Trends are statistical measurements of changes over time. The correct answer is "climate."

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which is true concerning the blue and magenta colors used to depict airspace on sectional aeronautical charts? group of answer choices faded lines represent airspace which extends to the surface.

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The given statement "the blue and magenta colors used to depict airspace on sectional aeronautical charts have faded lines which represent airspace which extends to the surface" is true because a sectional chart is a map utilized in air navigation that portrays the details of an area's airspace.

This map has contour lines and visual terrain characteristics, including obstructions, lakes, and rivers, which provide pilots with the information they need to navigate safely in VFR conditions.

The sectional chart's primary objective is to depict land features that might help a pilot navigate the area. The chart contains many different symbols and markings to indicate obstacles, airports, and other important details that a pilot should be aware of while flying. The colors blue and magenta are used to denote airspace on sectional charts.

Meanwhile, magenta color denotes airspace that stretches from the surface up to 10,000 feet, above sea level. It indicates Class E airspace in which Class G airspace above 14,500 feet MSL is also depicted in magenta. The faded lines within the blue and magenta airspace denote airspace that extends to the surface, as mentioned earlier.

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temperature, pressure, wind and moisture are measured through the depth of the troposphere by what instrument? group of answer choices rawinsonde doppler radar goes satellite

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Temperature, pressure, wind and moisture are measured through the depth of the troposphere using Rawinsonde instrument.

Rawinsonde is an instrument used to measure various meteorological parameters, including wind, temperature, and humidity. Rawinsonde is a balloon-borne instrument that is released into the air, and it sends back data as it rises. The balloon can rise to an altitude of around 100,000 feet before bursting, and the Rawinsonde instrument falls back to Earth. The data from the instrument are used to create a sounding, which is a profile of the atmosphere's temperature, pressure, and humidity as a function of altitude. The troposphere is the region of the atmosphere that is closest to the surface. It extends from the Earth's surface up to about 7-20 kilometers, depending on the latitude. The Rawinsonde instrument is used to measure the various meteorological parameters in the troposphere.

The Rawinsonde instrument consists of a weather balloon that is filled with helium gas. The balloon is released from the surface, and it rises through the atmosphere. As the balloon rises, the Rawinsonde instrument collects data on various meteorological parameters, including wind, temperature, and humidity. The data collected from the instrument are used to create a sounding, which is a profile of the atmosphere's temperature, pressure, and humidity as a function of altitude.

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further west from this deep u.s. trough, eastern alaska, as well as yukon and british columbia, canada, were being impacted by a . a. ridge b. trough g

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Further west from the deep U.S. trough, Eastern Alaska, as well as Yukon and British Columbia, Canada, were being impacted by a ridge.

A ridge of high pressure is impacting Eastern Alaska, Yukon and British Columbia in Canada, further west from the deep U.S. trough. A ridge of high pressure is an area of high atmospheric pressure, which is associated with fair weather, light winds and generally pleasant conditions. This ridge is formed when two air masses move away from each other, causing the air pressure in the area to increase. A ridge is typically indicated on a weather map by a line of red L's. The L's are placed on the map in the direction of the wind flow around the ridge, with the point of the L representing the area of highest atmospheric pressure.

The increased atmospheric pressure caused by the ridge produces lighter winds and warmer temperatures. The warmer temperatures and decreased wind speeds generally lead to more stable weather conditions and less precipitation. The ridge can also bring dry and sunny conditions, as well as a decrease in storm activity. These effects can be felt further downwind of the ridge, making it a welcomed feature in many areas.


In contrast, a trough is typically associated with low-pressure areas that produce wet, stormy weather conditions, as well as cool temperatures. This is because the low-pressure system promotes the formation of clouds and precipitation, which can reduce the amount of solar radiation that reaches the Earth's surface.

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most sediment on the continental shelf is derived from a. erosion on the continent b. life in the sea c. aliens d. chemical reactions in the water

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Chemical reactions in the water and aliens are not significant sources of sediment on the continental shelf. The correct option is d.

Most sediment on the continental shelf is derived from erosion on the continent.

What is the continental shelf?

The shallow oceanic area is known as the continental shelf.

It is located next to the shore and extends from the shore to the continental slope.

The water depth in the continental shelf ranges from 100 meters to 200 meters, depending on the location, and the slope of the shelf ranges from 0.1 to 1 degree.

The main source of sediment on the continental shelf is erosion on the continent.

When rocks and soil are exposed to the elements, such as wind, rain, and temperature fluctuations, they begin to erode.

This can result in sediment that is transported by rivers to the ocean and deposited on the continental shelf.

Other sources of sediment on the continental shelf include volcanic eruptions, underwater landslides, and other natural events.

Life in the sea is also a source of sediment, as organisms such as corals and clams produce shells and other materials that eventually break down and contribute to the sediment on the sea floor.

However, the primary source of sediment on the continental shelf is erosion on the continent.

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the giant planet that has an axis that points roughly straight up, and thus has no seasons to speak of, is:

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The giant planet that has an axis that points roughly straight up, and thus has no seasons to speak of, is Uranus.

Uranus is the giant planet that has an axis that points roughly straight up, and thus has no seasons to speak of. Uranus is the seventh planet from the Sun, and it was the first to be discovered by means of a telescope. It's also the third-largest planet in terms of diameter, and it's the fourth-most massive.

Uranus is also distinctive in that it is the only planet in the solar system that has an axis that is nearly perpendicular to the plane of its orbit. In addition, Uranus is primarily composed of hydrogen, helium, and methane, which accounts for its pale blue color. Uranus' atmosphere contains bands of clouds that are made up of methane crystals. The planet also has an extensive system of rings and a multitude of moons orbiting it.

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Which of the layers in the atmosphere do temperatures vary the most?

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Answer:

The Troposphere

Explanation:

It has most of our weather like rain, snow, and clouds.  On this part of the atmosphere, the temp gets cold as the amount of space above the earth increases.  

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