what is the approximate elevation at grid location 7-i?

Answer:

It Would be Texas be it says Stationary which means it Stays in the same place so 100% correct Promise

Explanation:

In the Northern Hemisphere, winter officially begins on December 21 and summer officially begins on June 21. (in the Southern Hemisphere).

The Tropic of Cancer (23°27′ N), the northernmost point of the Sun's vertical overhead beams, is reached on this day of the winter solstice in the Southern Hemisphere. Extreme weather and odd words to express it are characteristics of winter. At 6:12 a.m. The winter solstice, or the start of winter, occurs at approximately noon EST on Friday, December 21, when the sun crosses the Tropic of Capricorn, appearing to shine farthest south of the equator.

The only period when the quantity of sunlight and nightfall in the Northern and Southern Hemispheres is practically equal is during the equinoxes. Two equinoxes occur annually on Earth: one around March 21 and the other around September 22. The equator receives direct sunlight on March 21 and September 23. Since neither pole is oriented toward the sun in this configuration, there are equal numbers of days and nights on the entire planet. It is referred to as an equinox. The Northern Hemisphere is now experiencing a return to spring. In the Southern Hemisphere, the equinox in March signifies the beginning of fall and the equinox in September, the beginning of spring.

The longest day of the year in the Northern Hemisphere occurs on June 21; this day is known as the Summer Solstice. The length of a day in Delhi is roughly 14 hours. The latitudinal location of a site determines how much light it receives during the summer solstice in the Northern Hemisphere. The longest day of the year occurs in the hemisphere that is nearest to the sun, whereas the longest night occurs in the opposite hemisphere. The winter solstice occurs around 22 December and the summer solstice around 21 June in the northern hemisphere. In the southern hemisphere, these dates are reversible.

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The GLOBE (Global Learning and Observations to Benefit the Environment) study is a worldwide research initiative that involves students, teachers, and scientists collecting environmental data.

The study aims to enhance understanding of the Earth's systems and promote scientific literacy. The following outline provides an overview of the methodical procedure and key results of the GLOBE study:

Methodical Procedure:

a. Training: Teachers and students receive training on data collection protocols and measurement techniques.

b. Data Collection: Participants collect data in various environmental areas, including atmosphere, hydrology, soil, land cover, and phenology.

c. Protocols: The study provides detailed protocols and instruments for collecting and recording data.

d. Data Entry: Participants enter their collected data into the GLOBE database.

e. Quality Assurance: The collected data undergoes a rigorous quality assurance process to ensure accuracy and reliability.

f. Collaboration: The data is shared globally, facilitating collaboration among scientists, researchers, and educators.

Results:

a. Scientific Discoveries: The GLOBE study has led to numerous scientific discoveries and insights into Earth's systems, including climate patterns, weather phenomena, and ecological processes.

b. Education and Learning: Students and teachers involved in the study gain hands-on experience in scientific data collection and analysis, fostering scientific literacy and environmental awareness.

c. Global Network: The study has built a vast network of participants worldwide, promoting international collaboration in environmental research and education.

d. Data Availability: The collected data is freely accessible, allowing scientists and researchers to utilize it for further analysis, modeling, and understanding of global environmental processes.

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The term "porphyritic" refers to a rock that has massive crystals embedded in a matrix of smaller crystals.

Porphyritic rocks are distinguished by massive, well-formed crystals known as phenocrysts contained in a fine-grained matrix of smaller crystals. When lava cools slowly at deep, bigger crystals form first, allowing this type of rock to develop.

As a result, the surrounding matrix cools faster, resulting in smaller crystals. Porphyritic rocks are widespread in volcanic areas and are frequently utilized to establish how the rock developed. Numerous uses for porphyritic rocks exist, including buildings, ornamental stones, and monuments.

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Answer:

Constructive, destructive, conservative, and collision margins

Explanation:

These are the four kinds of plate margins.

A cold front, stretching across several states, is an example of synoptic-scale atmospheric motion.

Synoptic-scale refers to weather patterns and atmospheric motions that occur on a regional scale, typically covering an area of several hundred to a few thousand kilometers.

Synoptic-scale weather systems, such as cold fronts, are the result of interactions between large-scale atmospheric features, such as high and low-pressure systems, and the Earth's rotation.

In contrast, microscale atmospheric motion refers to very small-scale weather patterns, typically less than a few kilometers in size, such as the turbulence caused by a gust of wind.

Mesoscale atmospheric motion refers to weather patterns that occur on a larger scale than microscale but smaller than synoptic-scale, such as thunderstorms or sea breezes.

Global scale atmospheric motion refers to weather patterns and atmospheric motions that occur on a global scale, such as the jet stream or the movement of tropical cyclones.

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A hoodoo with a cap rock of sandstone and shale below is an example of differential weathering.

Differential weathering is the breaking down of rock, and erosion is the transportation of that broken rock, and these two natural forces work together to sculpt the hoodoos of a canyon. Ice and rain are the primary weathering and erosional forces that create the Hoodoos. A rock spire with a quickly eroded column and a more resilient cap that resembles mushrooms at times. They are eerie, so they are called "hoodoos," and they also go by other names, such as "fairy chimneys" and "goblins."

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Answer: early Europeans and people from Asia

Explanation: during the ice age it was thought that tribal people from the contanenet of europe and asia came to america via land briges in small tribal gruops these groups would later form many of the native american tribes we see today.

Answer:

May be C........ ....................

While winds above move air in a path that is almost parallel to the isobars on a weather map, surface winds often blow at an angle to them.

The reason why surface winds behave differently from winds aloft is best explained by FRICTION. A force called friction prevents a sliding object from moving. It is also the resistance of one object to motion as compared to another. It is not a basic force like electromagnetism or gravity. The electromagnetic attraction between charged particles in two touching surfaces, according to scientists, is what causes it. Additionally, it is the force that opposes the sliding motion of solid surfaces, fluid layers, and material components.

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Answer:

what is soil degradation

The land at creation likely consisted of one large supercontinent or multiple smaller land masses.

During the inception of the Earth, the land's composition presented two possibilities: a grand supercontinent uniting all landmasses or a patchwork of smaller land areas dispersed across the globe.

This geological enigma on intricate processes like tectonic plate dynamics, volcanic eruptions, and erosion over vast epochs. The notion of a supercontinent implies a united landmass before its eventual disintegration and rearrangement over geological epochs.

Conversely, the existence of multiple smaller land masses signifies a more fragmented and diverse planet, sculpted by a myriad of natural forces and processes during its ancient genesis.

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Most probably, your complete question is this:

Did the land at creation form one large supercontinent or multiple smaller land masses?

Decreasing the number of available frames increases the number of page faults, best describes Belady's anomaly. The correct option is A.

Belady's Anomaly is a phenomenon that occurs in virtual memory systems. It is a counterintuitive behavior in which increasing the number of available frames increases the number of page faults. This anomaly is caused by the locality of reference principle of virtual memory, which states that a program will tend to access memory locations that are close together.

When the number of frames is increased, the working set of a program is broken up into multiple frames. This causes the program to access more frames than it did before and thus creates more page faults. Additionally, decreasing the frame size increases the number of page faults because the same amount of memory is now spread out over a greater number of frames, thus creating more page faults.

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Volcanic activity created the fishing port that is important to the economy of the village of Vestmannaeyjar on the island of Heimaey, near Iceland.

Volcanic activity created the fishing port that is important to the economy of the village of Vestmannaeyjar on the island of Heimaey, near Iceland. Vestmannaeyjar is a volcanic island group located off the coast of southern Iceland. Vestmannaeyjar, often known as the Westman Islands, has become one of Iceland's major tourist destinations because of its distinct landscape and the abundance of natural features it has to offer.

Volcanic activity is known to produce a wide range of mineral resources that can be beneficial to human beings. Volcanic activity contributes to the formation of islands, mountains, lakes, and other natural features that can be exploited for economic purposes. For example, the fishing port in the village of Vestmannaeyjar on the island of Heimaey, near Iceland, was formed due to volcanic activity. As a result, the port has become one of the primary sources of economic activity for the island's inhabitants.

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It should be noted that tropical cyclones simply mean low pressure systems which form over warm tropical waters.

It should be noted that tropical cyclone simply means the intense circular storm which originates over warm tropical oceans.

Tropical cyclones usually form when the temperature of the sea surface is above 26.5°. It will dissipate when it moves over land.

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The earliest three eons of Earth's history, the Precambrian, lasted from roughly 4.6 billion to 635 million years ago. The Proterozoic, Archean, and Hadean eons make up the Precambrian period. The Proterozoic is the most recent aeon. 88% of Earth's history occurs during the Precambrian. So the C is the correct answer.

The word "Precambrian" is a colloquial term that is frequently used in scientific literature to refer to a significant portion of the Geological Time Scale, which spans from approximately 4.560 to 541 million years ago.

This time span equates to nearly 88% of the Earth's existence, with limits denoting the beginning of the Planet Earth and the appearance of fossils appropriate for systematic biostratigraphic correlation.

The name "Precambrian" has been used informally from the middle of the 19th century, right after the Cambrian Period was established, though its origin is unclear.

Hence, the correct answer is option C, 88 percent.

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Answer:

Longitudes

Explanation:

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Answer:

the American CBD is characterized by construction of skyscrapers

Answer:

Insolation is the amount of solar radiation that is received by a planet. Some of this energy is absorbed or reflected by the atmosphere, if there is one, and some reaches the surface.Terrestrial external radiation is due to the decay of radioactive materials in the earth itself. Terrestrial external radiation is created by the process of the natural breakdown—or radioactive decay—of radioisotopes in natural materials such as rocks, soil, vegetation, and groundwater.

Explanation:

In areas that were major centers of ice accumulation, the land has been slowly rebounding.

This phenomenon, known as glacial isostatic adjustment or post-glacial rebound, is the gradual rise of the Earth's crust in response to the removal of the weight of ice sheets that once covered those regions during the last ice age. It is a geophysical process that continues to occur over thousands of years after the retreat of glaciers.

During the last ice age, large ice sheets covered vast areas of land, exerting enormous pressure on the Earth's crust. As these ice sheets melted and retreated, the weight on the land was lifted, allowing the underlying crust to slowly rise in response to the removal of the ice load. This vertical movement of the land is known as post-glacial rebound or glacial isostatic adjustment.

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The worst possible location of an external surface flaw in a vessel would be at a highly stressed area, such as the mid-section or where the vessel experiences the maximum load.

The worst possible location of an external surface flaw in a vessel would be at a highly stressed area, such as the mid-section or where the vessel experiences the maximum load. In these areas, the presence of a surface flaw could potentially lead to a faster propagation of cracks and, ultimately, a failure of the vessel. Neglecting end effects, this mid-section would be the most critical area for an external surface flaw to occur.

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The worst possible location of an external surface flaw in a vessel would be at the point of maximum tensile stress, which typically occurs on the surface of the vessel perpendicular to the applied force or pressure.

In cylindrical vessels, this is typically at the mid-section of the vessel wall, where the stress is highest due to the bending caused by internal pressure. Therefore, if an external surface flaw were to occur at this point, it could potentially propagate and cause a catastrophic failure of the vessel.

It is important to note that other factors, such as the size, shape, and orientation of the flaw, as well as the material properties of the vessel, can also affect the likelihood and severity of failure.

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Answer:

Fold mountains are created where two or more of Earth's tectonic plates are pushed together. At these colliding, compressing boundaries, rocks and debris are warped and folded into rocky outcrops, hills, mountains, and entire mountain ranges. Fold mountains are created through a process called orogeny

Answer:

O peer-reviewed journal

Explanation: mark me brainliest!!

Where scientists report their results and other scientists review their work to make sure they followed the scientific method.

Answer:

387

Explanation:

430% of 90 = 90*4.3 = 387

The observable characteristics of equinoxes and solstices in the continental United States are as follows:

1. Equal Day and Night (Approximately 12 hours of daylight and 12 hours of darkness)

2. Varying Lengths of Daylight

3. Changing Sun Angle and Altitude

4. Shifting Sunrise and Sunset Times

1. Equal Day and Night: This characteristic corresponds to the equinoxes, which occur in March (spring equinox) and September (autumn equinox). During these times, the Earth's axis is neither tilted away from nor towards the Sun, resulting in nearly equal lengths of daylight and darkness.

2. Varying Lengths of Daylight: This characteristic is associated with the solstices. The summer solstice, which falls around June 21st, marks the longest day of the year in terms of daylight hours. Conversely, the winter solstice, around December 21st, represents the shortest day of the year with the least amount of daylight.

3. Changing Sun Angle and Altitude: The solstices are responsible for the changing sun angle and altitude. During the summer solstice, the Sun appears higher in the sky, resulting in a steeper angle of incidence and more direct sunlight. In contrast, the winter solstice brings a lower Sun angle and reduced sunlight due to the tilt of the Earth's axis.

4. Shifting Sunrise and Sunset Times: Both the equinoxes and solstices contribute to shifting sunrise and sunset times throughout the year. During the solstices, these times reach their extreme points. For example, the summer solstice has early sunrises and late sunsets, while the winter solstice experiences late sunrises and early sunsets. The equinoxes mark the midpoint between these extremes.

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The Andes Mountains the oceanic trench, and numerous volcanoes and earthquakes on the western side of South America indicate that this is a(n) subduction zone.

What is a subduction zone?Subduction zones are areas where one tectonic plate is descending beneath another. Subduction zones are areas of intense seismic activity which can result in significant earthquake and volcanic activity. The Andes Mountains the oceanic trench, and numerous volcanoes and earthquakes on the western side of South America indicate that this is a subduction zone.

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Answer:

because it permits certain movement of molecules in and out of the cell

Answer:

a

Explanation: