What does the nishan sahib symbolize on top of the flag post?
A.
khanda
B.
Ik Onkar
C.
kirpan
D.
karra

Answer:The Carthaginians were Phoenicians, which means that they would conventionally be described as a Semitic people.

Explanation:

Answer:

Tension causes rocks to lengthen or break apart. Tension is the major type of stress found at divergent plate boundaries. Shear stress happens when forces slide past each other in opposite directions (Figure below). This is the most common stress found at transform plate boundaries.

Answer:

Migration is the movement and in human terms usually means a change of home.

Explanation:

hope this helps....

The principles of stratigraphy alone will not allow you to determine an absolute age of a fossil or rock.We are unable to identify a fossil's or rock's exact age using the stratigraphic concepts alone.

Stratigraphy is the study of the relationships between rock layers, or strata, and it helps to determine relative ages. However, further procedures and methodologies are needed to calculate the absolute age, which is the real age in years.

Using principles like superposition (younger rocks are typically on top of older rocks), original horizontality (sedimentary rocks are first deposited in horizontal layers), and cross-cutting relationships, stratigraphy aids in determining the relative order of rock layers and fossils within them.

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Explanation:

Natural hazard: an extreme event that can cause extreme damage to property, disrupt human activities and cause loss of life e.g. flooding.

Tectonic hazards basically happen when the earths crust moves. For example when the plates move there's friction which can cause them to become stuck and tension builds until the plates release, this leads to an earthquake. weather hazards happen when a regain has certain weather conditions like really heavy rain fall can lead to flooding.

convection currents occur because there's heat rising and falling inside the mantle.

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Answer:

Cubre un área de 8.515.767 km.

Explanation:

The change in volume of the neon gas when a 0.25 mol sample of neon gas at 18 °C and 0.799 atm is heated to 49°C and the new gas pressure is 1.11 atm can be calculated using the combined gas law which states that the pressure of a gas is proportional to its temperature and inversely proportional to its volume.

Using the formula of the combined gas law, we can express the relationship between the initial and final volume, pressure and temperature of the neon gas as shown below:

(P1V1) / T1 = (P2V2) / T2

Substituting the given values, we have:

(0.799 atm × V1) / (18 °C + 273) K = (1.11 atm × V2) / (49 °C + 273) K

Simplifying, we get:

V2 = (0.799 atm × V1 × (49 °C + 273) K) / (1.11 atm × (18 °C + 273) K)

V2 = (0.799 × V1 × 322 K) / 1.11 × 291 K

V2 = (231.988 V1) / 320.01

V2 = 0.724 V1

Hence, the change in volume of the neon gas is -0.276 times its initial volume. This means that the final volume of the gas is approximately 27.6% less than its initial volume.

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The main focus of the study "A Full-Stokes 3-D Calving Model Applied to a Large Greenlandic Glacier" was to investigate the calving processes of a specific glacier in Greenland using a comprehensive 3D model.

In this study, Todd applied a full-Stokes 3D calving model to a large glacier in Greenland to understand and simulate the mechanisms and processes involved in glacier calving. The study aimed to improve our understanding of how ice breaks off from the glacier front and contributes to sea-level rise.

By using a full-Stokes 3D model, which takes into account the complex physics of ice deformation, stress distribution, and fracture mechanics, the study aimed to provide more accurate and detailed insights into calving processes. The model allowed the researchers to simulate the behavior of the glacier, including factors such as ice flow, crevasse formation, and iceberg detachment.

The findings of the study contribute to our knowledge of glacier dynamics and the factors influencing calving events, which are essential for predicting and understanding the response of glaciers to climate change. The research provides valuable information for improving models used to assess future sea-level rise and to evaluate the impacts of glacier retreats in Greenland and other regions experiencing rapid ice loss.

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Answer:

Here you are

Explanation:

It's actually easy, you have just to write everything you know and then look if there's an angle between two sides or vice versa.

Siltstone, sandstone, and conglomerate are more prone to slipping along bedding planes due to their rounded particles, which allow for easier movement between layers. Clay particles in shale, on the other hand, tend to line up and adsorb water, making them more prone to stick together and be less likely to slip along bedding planes.


The type of rock that would be more prone to slipping along bedding planes would be shale. This is because the clay particles that make up shale tend to line up in the same direction during the lithification process, creating a weak plane along which the rock can slip. This can be especially problematic if the bedding plane is inclined or if there is water present, which can further reduce the strength of the rock.On the other hand, siltstone, sandstone, and conglomerate are made up of rounded particles that are typically more tightly packed and less likely to slip along bedding planes. The shape and size of these particles make them more resistant to shearing forces and less likely to deform under pressure.As for the type of rock that would have the least strength, it would also be shale. This is because clay particles are generally weaker and less resistant to pressure than rounded particles. Additionally, the lining up of these particles in the same direction creates a weakness in the rock that can further reduce its strength.In conclusion, shale is more prone to slipping along bedding planes and has the least strength due to its composition of weak and easily deformable clay particles. Siltstone, sandstone, and conglomerate, on the other hand, are less prone to slipping and have greater strength due to the shape and size of their rounded particles.

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Answer:try your best

Explanation:

Ultisols are the most common soil order in portions of North America, where annual precipitation ranges from 60 to 79 inches.

There are twelve different soil orders in the US, and ultisols are one among them. This soil order is predominantly found in North Carolina, which is located in the northern region of the United States. In this area of North Carolina, there are 60 to 79 inches of annual rainfall on average.

Ultisols are particularly likely to be found in humid regions or tropical areas. The ultisols are characterized by their dry and red clay soils as well as by their capacity to weather materials in humid and temperate environments.

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Answer:

Erosion breaks existing rocks and turns them into sediments. The sediments can be formed into rocks by the chemical reactions of dissolved seashells ( Calcium Carbonate.) This reaction can form sediments into rocks very quickly like the formation of concrete ( same chemical reaction). Erosion only happens on the earth's surface.  

As erosion only happens on the earth's surface, sedimentary rocks are only formed on the earth's surface.

In other words:

Sedimentary rocks only found on or close to Earth's surface because sedimentary rocks are made of materials deposited in layers at the Earth's surface.

The eye of a hurricane has all of the following characteristics, except heavy rain; and it is turning as a result of the Earth’s rotation about its axis. The correct options to complete the statement are relatively clear skies and relative vorticity.

The center of a hurricane has a calm zone of low pressure known as the eye. It is distinguished by light winds, relatively clear skies and descending air. However the surrounding eyewall experiences storm surge, powerful winds, and heavy rain.

The Coriolis effect which is caused by the Earth's rotation about its axis, is what causes hurricanes to turn. As a result the hurricane begins to rotate in the Southern Hemisphere in a clockwise direction and the Northern Hemisphere in a counterclockwise direction. Relative vorticity is a term used to describe this rotation.

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Answer: J. 31, 43

Explanation:

55 - 19 = 36

Then 36 ÷ 3 = 12

So then 19 + 12 = 31

and 31 + 12 = 43.

Finally 43 + 12 = 55.

Answer:

B is right just got 100% pls mark brainliest

Explanation:

In the past 3.2 billion years, Earth had about 190 major impacts (i.e., impacts leaving craters greater than 25 km in diameter).

These impacts were caused by asteroids or comets colliding with the Earth's surface, and they have had a significant impact on the planet's geological history. Some of the most well-known impact craters include the Chicxulub crater in Mexico, which is believed to be the result of the asteroid impact that caused the extinction of the dinosaurs, and the Vredefort crater in South Africa, which is the largest known impact crater on Earth.

While these impacts can have devastating effects on life on Earth, they have also played a crucial role in shaping the planet's surface and atmosphere over time. Scientists continue to study these impacts in order to better understand the history of our planet and the potential risks posed by future impact events.

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Islam is growing faster than any other religion.

In fact, some demographers believe that around

the year 2070, muslims will outnumber christians.

Christian populations are still growing, but not

nearly as fast to keep up with the pace of muslims.

Answer:

mediterranean sea  OKAy

Answer:

The Mediterranean Sea

Explanation:

The Strait of Gibraltar connects the Atlantic Ocean with the Mediterranean Sea and separates Spain on the European continent from Morocco on the African continent.

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In sedimentation equilibrium, the shape of the final concentration gradient is solely dependent on the size and shape of the protein.

Sedimentation equilibrium is a method of analyzing the relationship between a macromolecule's molecular weight and its sedimentation coefficient. A centrifuge is used to perform the experiment, which separates particles based on their sedimentation coefficient and measures their concentration at the bottom of the test tube.In other words, it's the process of obtaining information about a particle's mass and shape by measuring its settling velocity and the equilibrium distribution of the concentration gradient.

Therefore, the shape of the final concentration gradient is solely dependent on the size and shape of the protein. Sedimentation equilibrium provides an accurate determination of a macromolecule's weight-averaged molecular weight and shape. It helps researchers investigate biological macromolecules, especially large proteins and nucleic acids, by determining their molar masses and sizes.

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Surface runoff and sediment yield will decrease with the increased effectiveness of a protective vegetation cover.

When an area is left uncovered, rainwater hits the ground with force and can cause soil erosion. Soil particles are dislodged and are carried away by the water, creating sediment yield that can negatively impact water quality and aquatic life downstream.

A protective vegetation cover, on the other hand, can help reduce the impact of rainwater on the soil surface. The roots of the plants hold the soil in place and prevent erosion.

Additionally, the leaves and branches of the plants intercept and slow down rainfall, allowing it to soak into the ground more slowly and reducing the amount of runoff.
Studies have shown that a dense and diverse vegetation cover can significantly reduce surface runoff and sediment yield. This is because the vegetation cover can increase infiltration rates and reduce soil erosion rates.

Moreover, vegetation can also help reduce the amount of pollutants that are transported by surface runoff, which can further improve water quality.
Overall, the effectiveness of a protective vegetation cover can significantly reduce the negative impacts of surface runoff and sediment yield.

As such, planting vegetation is an important strategy for managing soil erosion and improving water quality in our rivers and streams.

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Answer:

It could be business

Explanation:

Well if you think about it, band won't help him with farming and i don't think history would either. Physics is basically physical science, so I don't think that's it either. I hope this helps. God bless!

Answer:

D) Coordinate placement

Explanation:

From north to south is 180 and same with east and west

The unsaturated zone is above the saturated zone. A gushing well is likely an artesian well. Darcy's Law relates discharge to various factors.

Above the saturated zone is the unsaturated zone. It is the area where the soil or rock has both air and water, but the pores do not have enough water to fill them completely.

It is most likely an artesian well if you see a well bore hole spewing water. By applying pressure to a confined aquifer, artesian wells cause water to flow to the surface naturally without the use of pumps.

According to Darcy's Law, the hydraulic gradient (dh), cross-sectional area (A), and hydraulic conductivity (K) all influence discharge (Q). You can write it out as Q = K × A × dh. In light of Darcy's Law, all of the given options (DI, K, A, and Dh) are accurate.

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Answer:Correct

Explanation:Correct

Answer:

B and C

Explanation:

so so soryy if im wrong

Explanation:

I guess the answer is B and D

from which I know, D is for sure

Answer:

Dear canoeist,

I would like to advise you that it is not recommended to follow the inner banks of the river in this course of the river. This is because there might be obstacles or currents that can make rowing difficult and even put you in danger. The outer banks are usually less steep and have less undercurrent, making it easier to navigate the river safely. Additionally, following the inner banks might also disturb the natural ecosystem of the river, which can have negative consequences. It is essential to keep yourself and the river safe by following the recommended path, which usually means not sticking to the inner banks.

Best regards,

Drake

I hope this answers your questions

There are a few reasons why it is not recommended for canoeists to follow the inner banks of a river in certain courses.

The current is stronger: The inner banks of a river are often where the current is strongest. This is because the water is constricted by the banks, so it has to flow faster to get through. This can make it difficult for canoeists to control their boats, and it can also increase the risk of capsizing.

There are more hazards: The inner banks of a river are often where there are more hazards, such as rocks, debris, and underwater stumps. These hazards can damage a canoeist's boat, and they can also pose a safety risk.

The view is obstructed: The inner banks of a river often obstruct the view of the river ahead. This can make it difficult for canoeists to see what is coming, and it can increase the risk of collisions.

So, it is generally recommended for canoeists to follow the outer banks of a river whenever possible. The outer banks are often where the current is weaker, there are fewer hazards, and the view is better.

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Answer: D. Timor

Explanation: