3. If mzFx = 2x+9 & mzEFK = 5x + 4. Find
the measurement of m?
3
E
A. 11
B. 31
C. 59
D. 90-

Answer:

A Right triangle

Explanation:

A^2+B^2=C^2

Answer: right triangle

Explanation:

Answer:

it is d

Explanation:

It is d because mid ocean ridges are close to or have some sort of volcanic activity

the Veldic religion evolved and spread

Answer:

A rock with a half-life of 5,280 years having 1/8th of the parent material left will be 15,840 years old.

Explanation:

The half-life of a material is the time needed for only half of the parent material to be left, while half has is gone, or rather has disintegrated. The half-life is used further into the falling apart of the parent material though, with the same principle being applied. Practically, from the 1/2 of the parent material being left, the half-life of it would mean 1/4 of the parent material being left, and from that 1/4, the half-life would be at 1/8 of the parent material being left, and so one, by simply dividing in two.

In this case, having a half-life of the rock of 5,280 years, we will simply need to add that amount of years on every next phase. So, the half-life is 5,280 when 1/ of the parent material is left. When 1/4 of the parent material will be left we will have an age of 10,560 years, while when only 1/8 is left, we will have 15,840 years of age for the rock.

The Earth has distinct layers, with the inner core being the most solid, the outer core being liquid, and the mantle and crust being solid. These layers resulted from the Earth's molten state.

The Earth was molten when it first formed. As it began to cool, it began to separate into layers. The denser materials, such as iron and nickel, sank to the center to form the core. Lighter materials, such as silicon and oxygen, floated to the surface to form the crust. The Mantle, the thickest of the Earth's layers, sits above the core. It is composed of hot, dense rock, and is responsible for much of the Earth's volcanic and tectonic activity. The outer core, which surrounds the inner core, is made up of liquid metal and creates Earth's magnetic field. The crust, which is the outermost layer, is divided into plates that move and interact with each other, causing earthquakes, volcanic eruptions, and mountain formation. The reason for this layering is due to the differences in density among the materials that make up the Earth. The heavier elements sank to the center to form the core, while the lighter elements floated to the surface to form the crust.

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Answer:

it would be 86 degrees as a fahrenheit if that is what you were asking

Explanation:

The large area of flat land in the Midwest portion of the United States is known as the Great Plains.

This region stretches across the central part of the country, from Texas in the south to the Dakotas in the north. The Great Plains are characterized by their vast grasslands, which were once home to millions of bison. Today, the region is an important agricultural area, producing crops such as wheat, corn, and soybeans.

The Great Plains are also known for their extreme weather, including tornadoes, blizzards, and droughts. Despite these challenges, the region has a rich history and culture, shaped by the people who have called it home for thousands of years.

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Answer: Red dwarfs

Explanation:

Red dwarfs are thought to be the coolest star out of the rest. They are also the smallest. Because they are so cool, their luminosity is low as well on account of the fact that relatively speaking, the fusion taking place on their surface is little.

Red dwarfs are the most numerous star in the universe and the most numerous in the Milky Way galaxy as well. We just can't see them with out naked eyes because of their low luminosities.

Answer:

Atlantic and Pacific

Explanation:

Atlantic ocean surrounds on east and Pacific ocean on west

Answer:

Water temperatures increase because the trees that provide cover from sunlight are cut down. All of these factors disrupt a river ecosystem because the species that live in the stream have adapted to conditions before the deforestation and may be negatively impacted by the sudden changes.

Explanation:

Answer:

The water temperatures would increase because without trees, the sunlight shines on the water which makes it hotter.

Explanation:

Water temperatures increase because the trees that provide cover from sunlight are cut down. All of these factors disrupt a river ecosystem because the species that live in the stream have adapted to conditions before the deforestation and may be negatively impacted by the sudden changes.

Answer:

Explanation:

Explain why many farmers were dissatisfied with Nazi policies towards agriculture. (12 marks) There were multiple reasons why the farmers in Nazi Germany were dissatisfied by the Nazi policies towards agriculture. This was based upon the fact that the farmers wages had dramatically dropped behind those of the industrial workers.

Answer:

Sandy Beaches

Sandy beaches are the most common of all beach types in the world, and they are found in virtually all continents on earth. This type of beach occurs typically on coasts which experience low-energy waves, which deposit the sand to the beach after being transported by ocean currents. Sandy beaches are most susceptible to backwash erosion, with powerful storms and tsunamis having the potential of stripping a beach of its sand. To remedy the erosion of the sand drastic measures have been employed including beach nourishment where sand is sourced from other places and deposited on the beach.

Pebble Beaches

Pebbles are found on virtually all beaches on earth. However, there are a few beaches in the world that are entirely composed of pebbles, which are known as pebble beaches. The pebbles that cover these beaches vary in size, ranging between 0.1 and 7.9 inches in diameter with the larger pebbles often being found nearer to the shore. Pebble beaches are formed after pebbles carried by ocean currents are deposited on the shore by high-energy waves. Pebble beaches are excellent in the prevention of backwash erosion and dissipation of wave energy due to their porous nature. Pebble beaches are picturesque, and since they are not as popular among tourists as sandy beaches, they are less-crowded making them ideal for a private beach experience. Also known as shingle beaches, this type of beaches is popular among rock collectors, who collect the smooth pebbles which are used in exterior and interior decorations of homes.

Boulder Beaches

Boulder beaches are so named due to the boulders that cover their shorelines. The size of the boulders found on boulder beaches ranges from tiny pebbles to huge house-sized boulders. An example of a boulder beach is the Valugan Boulder Beach, which is covered with boulders. Situated in Batanes, Philippines, the beach is one the true boulder beaches in the world, as the shoreline is entirely made up of boulders.

Shell Beaches

As the name alludes, a shell beach is almost entirely made up of shells. The shells that cover these beaches are mainly from dead mollusks and are deposited on the shore by waves. In some of the beaches, the shell layer can be dozens of feet in depth. Examples of this type of beaches are quite a few and only two exist that are true shell beaches which are Australia’s Shell Beach and Sanibel Shell Beach of the United States. Shell Beach, Australia is one of the two legitimate shell beaches in the world, as it is purely composed of shells. The beach is situated in Western Australia’s Shark Bay which lies about 28 miles from the town of Denham.

Sea Glass

Sea glass is another substance that covers some of the earth’s beaches. Sea glass forms after broken glass disposed of in the sea are acted upon by erosion action, which over time smoothens its sharp edges to result in a piece of glass with smoothened and rounded surface. There are no beaches that are entirely composed of sea glass, due to the small quantities of sea glass that occurs naturally in the earth’s oceans. However, there are a few beaches where large quantities of sea glass cover the surface. Bermuda’s Black Bay Beach is one beach that is covered by sea glass.

One reason for the westward boundary intensification of boundary currents has to do with the intensification of the Coriolis effect with latitude. The Coriolis effect is stronger at western latitudes than at trade wind latitudes.

The Kuroshio is the western boundary current of the subtropical gyre in the North Pacific and requires comparison with its Atlantic counterpart, the Gulf Stream.

The Western Boundary Current is a strong, narrow current confined to the western side of the basin. In the North Atlantic, the Gulf Stream is the western boundary current of the anticyclonic subtropical gyre, and the North Atlantic Current (NAC) is its northeastern extension (Arhan, 1990; Rossby, 1996).

In fact, they are one of the fastest surface currents in the ocean. One reason for the westward amplification of boundary currents has to do with the amplification of the Coriolis effect with latitude. The Coriolis effect is stronger at western latitudes than at trade wind latitudes.

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An economic system based on traditional agriculture is Barter system .

During the ancient times people don't have money to purchase the goods , so they invent a traditional exchange system known as barter system .  It is act of trading goods or services between two or more parties without the use of money. For instance let say a farmer needs a pair of shoes from a shoemaker , so he exchanges with a bushel of wheat , farmer gets the shoes and shoemaker gets the bushel of wheat, but this system requires requires the double coincidence of wants.

This is how people used to trade via barter system.

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Answer:

Scalar quantity

Explanation:

Scalar quantities give a magnitude, while vector quantities give a magnitude and a direction. The answer will be a measurement that does not change, regardless of the direction of action. Displacement is a measure of length in a given direction; distance is the scalar version of displacement. hence length is scalar quantity

This is due to the fact that the Earth's surface absorbs and re-emits shortwave radiation from the Sun, causing the air near the surface to heat up faster than the air at higher altitudes. As a result, the temperature difference between the surface and the air aloft increases, leading to a steeper environmental lapse rate.

The lower atmosphere typically has a steeper environmental lapse rate in the middle of the day because the surface warms more rapidly than the air aloft. This is due to the fact that the atmosphere is heated from the ground up, and the surface is in direct contact with the sun's shortwave radiation. As the surface heats up, it transfers some of its heat to the air above it, but the air aloft tends to be cooler and less affected by the sun's radiation. Therefore, there is a greater temperature difference between the surface and the air aloft, which leads to a steeper environmental lapse rate.

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The correct order of the processes that occur when oceanic plates spread apart at the mid-ocean ridge, from the first event at the top to the last event at the bottom, is as follows: Cracks appear in the oceanic plates .Lava rises and hardens. The mid-ocean ridge rises up from the ocean floor.

Tectonic plates diverge and move away from each other, leaving a gap in between .The oldest rocks move away from the mid-ocean ridge, while new rocks are formed near the mid-ocean ridge. This occurs at the boundary between the plates on both sides of the mid-ocean ridge.

The mid-ocean ridge is the largest mountain range in the world. It is a chain of submarine mountains that runs across the middle of the ocean, with a crack running down the center. New oceanic crust is formed at the mid-ocean ridge, and old crust is destroyed at subduction zones.

The process by which new oceanic crust is created is called seafloor spreading. As the oceanic plates move apart, magma rises from the mantle and hardens into solid rock, forming new crust on both sides of the ridge.

Cracks appear in the oceanic plates at the mid-ocean ridge, and lava rises from below to fill them.

This lava hardens into solid rock, forming a new layer of oceanic crust. Over time, the oceanic crust moves away from the mid-ocean ridge, and new crust is formed in its place. Over time, the oceanic crust moves away from the mid-ocean ridge, and new crust is formed in its place.

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Earthquakes and volcanoes do not occur in random locations around the world. Instead, they usually only appear along specific zones or belts.

These belts are found near plate boundaries, as scientists realised after learning about plate tectonics.

Broad sense foreshocks, preseismic quiescence, precursory swarms, and doughnut patterns are a few of them. Although all or some of these patterns precede numerous earthquakes, their specifics vary greatly from event to event.

The Circum-Pacific Belt, often known as the Ring of Fire, is a region along the Pacific Ocean marked by active volcanoes and frequent earthquakes. The Ring of Fire is where most of Earth's earthquakes and volcanoes occur.

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The statement is true because, according to general relativity, space is indeed warped or curved by matter.

General relativity, a theory developed by Albert Einstein, describes gravity not as a force but as a curvature in spacetime caused by the presence of mass. This means that any object with mass, such as a planet or a star, will cause a distortion in the fabric of spacetime around it.

As a result, other objects moving through this curved spacetime will experience what we perceive as gravitational attraction. This theory has been confirmed through various experiments and observations, such as the bending of light around massive objects like the sun during a solar eclipse.

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Increased absorption of atmospheric carbon dioxide in surface waters of the oceans forms carbonic acid, which in turn lowers the pH of seawater.

The carbonic acid formed when carbon dioxide dissolves in seawater reacts with water molecules to produce hydrogen ions (H+) and bicarbonate ions (HCO3-).

This increase in hydrogen ions decreases the pH of seawater, making it more acidic. This process is known as ocean acidification, which has significant impacts on marine organisms and ecosystems, particularly those with calcareous structures such as shells and coral reefs, which are particularly vulnerable to dissolution in acidic conditions.

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Answer:

A. Most of the moisture is captured in the mountains, where it falls

as snow.

Explanation:

A. Most of the moisture is captured in the mountains, where it falls

as snow.

When monsoons hit the Himalayan mountain range, most of the moisture is captured in the mountains, where it falls as snow. This snowfall helps to replenish the water supply in the region. Additionally, rain levels increase dramatically in eastern China, while wind and rain are redirected to the east, to Southeast Asia, and to the west, into Pakistan and Iran. This helps to bring much needed moisture to these areas, which can help to support local agriculture and ecosystems. The monsoon season in the Himalayas is an important part of the region's water cycle and helps to sustain the local environment.

The United States National Park with sedimentary rocks, metamorphic rocks, and a history of flooding is the Yosemite National Park.

Yosemite National Park is home to some of the world’s most iconic landforms, including Yosemite Valley and Yosemite Falls. The park’s landscape owes its beauty to the area's unique geology, which results from the glacial erosion of its underlying granite.

Some of the most iconic landforms in Yosemite National Park are Yosemite Falls, Yosemite Valley, and Yosemite Valley Falls. Other iconic landforms include El Capitan, El Capitan Falls, Half Dome, Cathedral Peak, and many more. In addition to their natural beauty, Yosemite National Park’s iconic landforms are also significant sites for studying and understanding the Sierra Nevada’s geological history.

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Answer: drains storm water from three square miles.The west fork headwaters drain part of The Ridges of Park wood, part of Park wood Village.

Explanation:

Answer:The ready access to vast areas of the Atlantic Ocean and a number of major seas, lakes, and rivers has made fish an important natural resource in Europe. The seas around Europe provide about ten percent of the world’s fish catches. Mirroring the situation around the world, European fishing activity increased as the population increased. Europeans are becoming increasingly aware of the effects of overfishing. Stocks of Atlantic cod and Atlantic mackerel are considered to be at risk because of the threats of overfishing and changes in the environment that are affecting natural mortality and slowing spawning. The ready access to vast areas of the Atlantic Ocean and a number of major seas, lakes, and rivers has made fish an important natural resource in Europe. The seas around Europe provide about ten percent of the world’s fish catches. Mirroring the situation around the world, European fishing activity increased as the population increased. Europeans are becoming increasingly aware of the effects of overfishing. Stocks of Atlantic cod and Atlantic mackerel are considered to be at risk because of the threats of overfishing and changes in the environment that are affecting natural mortality and slowing spawning.

Explanation:

The Common Fisheries Policy (CFP) is the EU's fisheries strategy (EU). In addition to establishing quotas for member states to catch different species of fish, it also supports the fishing industry through a variety of market interventions.

It provides a significant amount of food to many nations around the world, but those who engage in it professionally frequently have to pursue fish in dangerous ocean conditions and at great distances. Commercial fishing on a large scale is also referred to as industrial fishing.

The effects of overfishing are becoming better known to Europeans. Threats from overfishing and environmental changes that are slowing spawning and affecting natural mortality have led to the designation of stocks of Atlantic cod and Atlantic mackerel as being at risk.

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8 million gallons of oil spills were leaked into the nearby waterways harming the ecosystem of the gulf coast and additionally causing destruction to the habitat.

One of the most damaging hurricanes in American history, Hurricane Katrina made landfall on the Louisiana coast on August 29, 2005.  Nearly 92,000 miles of the Gulf Coast were affected by Katrina, a Category 3 storm that made landfall with gusts of above 120 mph. Over 800,000 people were forced to leave their homes as a consequence of the destruction, which cost upwards of $81 billion. Around 1,800 people lost their lives as a result of the damage. Nearly 8 million gallons of oil were leaked into nearby waterways as a result of oil spills from three different refineries, further harming the ecosystems in the area. Another regrettable effect of Hurricane Katrina was the destruction of habitats along the Gulf coast.

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