below is a photograph of part of the grand canyon that has seven geologic events labeled with letters. please use the geologic laws of relative dating to order these events from the first event that occurred to the last event that occurred.

The correct answer is Following are all of his Phil outcomes since 1887: (Six more weeks of winter) Saw shadow: 106. (Early spring) No shadow: 29. Shadowing in part: 1.

The National Oceanic and Atmospheric Administration discovered that, on average, Punxsutawney Phil was 40% accurate when comparing his prognosis to the national weather for the previous ten years. Folklore holds that if he sees his shadow, there will be another six weeks of winter. If not, spring arrives before schedule. Phil could see his shadow this time. A group of local dignitaries known as the "inner circle" are in charge of organising the activities as well as providing Phil with food and care. Since making his initial prognostication in 1887, the groundhog has consistently seen his shadow three years in a row.

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The document you are referring to is commonly known as the "Zoning Ordinance" or "Zoning Code."

The Zoning Ordinance is a set of regulations that governs land use and development within a city or county. It establishes specific guidelines and standards for different zones or districts within the jurisdiction. These zones are typically categorized based on the type of land use allowed, such as residential, commercial, industrial, or mixed-use.

The purpose of a Zoning Ordinance is to promote orderly growth and development, protect the character of different areas, ensure compatibility between land uses, and address public health, safety, and welfare concerns. It typically includes provisions related to building heights, setbacks, lot sizes, parking requirements, and other factors that determine how land can be utilized.

The Zoning Ordinance is often considered the constitution for land use within a city or county because it sets the legal framework for how properties can be used and developed. It guides landowners, developers, and government officials in making decisions regarding land use, building permits, and zoning variances.

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Answer:

True

Explanation:

Hot, I took the test :)

Labor market facts can help determine preferred locations for work based on job growth, industries, unemployment rates, and salaries.

While considering geology and area for finding work, it is essential to figure out where you need to be and assuming you are limited by area or then again on the off chance that it sets out new open doors. Obtaining work market realities can give motivation to your decisions.

For instance, to work in a particular city or district, you can explore the work market measurements for that area. This can remember data for work development, businesses pervasive in the locale, joblessness rates, and normal compensations.

Sources, for example, government sites, work market reports, and industry-explicit distributions can give important experiences into the work market elements of various areas.

By looking at these work market realities, you can survey the accessibility of open positions, the seriousness of the market, and the potential for vocation development in your ideal area. This data can assist you with settling on informed conclusions about where to concentrate your pursuit of employment and target businesses or areas that line up with your abilities and interests.

Make sure to refer to and reference the sources you use to give precise and solid data in your work statistical surveying.

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To estimate the years of accumulated strain released during the Fort Tejon earthquake, we would need the average rate of fault movement calculated in problem 1b, as mentioned in the question. Unfortunately, the content provided does not include the information from problem 1b. Without that specific data, we cannot make a precise calculation.

However, I can provide a general explanation of how the estimate could be derived based on the average rate of fault movement. The average rate of fault movement represents the speed at which tectonic plates are accumulating strain along the fault line. By multiplying this rate by the offset distance of 10.0 meters (33 feet), we can estimate the time it took to accumulate that amount of strain.

For example, if the average rate of fault movement is 1 centimeter per year, we can convert the offset of 10.0 meters to centimeters (1000 centimeters) and divide it by the average rate of fault movement (1 centimeter per year). This would give us an estimate of 1000 years to accumulate that amount of strain.

However, it is important to note that this estimation is based on a simplistic assumption and may not reflect the actual complexities of fault behavior and strain accumulation. Detailed geological studies and data analysis are necessary for a more accurate assessment of accumulated strain and earthquake recurrence intervals.

Without the specific average rate of fault movement from problem 1b, we cannot provide a precise estimate of the years of accumulated strain released during the Fort Tejon earthquake.

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Answer:

1.mesosphere is a coldest atmospheric layer surrounfing the earth

2.it become cloud enough to freeze water vapour

3.the ice cloud are blue white are caled noctilucent

Explanation:

Answer:

A

Explanation:

Answer:

https://odihpn.org/magazine/emergency-interventions-in-the-arid-and-semi-arid-areas-of-northern-kenya/

Explanation:

i'v attached a link that gives you all the information you need to formulate an answer

To compute the runoff volume for the catchment, we need to consider the following factors: 1. Convert the catchment dimensions from feet to meters: 1500 feet = 457.2 meters, 1000 feet = 304.8 meters.

2. Determine the area of the catchment: Area = Length x Width = 457.2 meters x 304.8 meters = 139,354.56 square meters. 3. Calculate the runoff coefficient (C): The average curve number (CN) for the catchment is 65. Runoff coefficient can be estimated using the formula: C = (CN - 10) / (CN + S), where S is a soil retention parameter (assumed as 254 / CN in this case).

\(C = (65 - 10) / (65 + (254/65)) = 0.434. 4\). Calculate the effective rainfall (R): The depth of rainfall is 5 inches, which is approximately 0.127 meters. Effective rainfall (R) can be estimated by the equation: R = P - (Ia + S). Assuming initial abstraction (Ia) as 0.2S and surface storage (S) as 0.05S, \(R = 0.127 - (0.2 * S + 0.05 * S) = 0.127 - (0.2 + 0.05) * S = 0.127 - 0.25S. 5.\)

Calculate the runoff volume (V): The runoff volume (V) can be calculated using the equation: V \(= C * R * A. V = 0.434 * (0.127 - 0.25S) * 139,354.56.\) By incorporating pounding and recharge measures, the flood risk can be mitigated to some extent. However, without specific information on the measures being adopted, it is difficult to assess the magnitude of risk reduction accurately.

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Answer:

1. are extint.........

Answer:

1).are extinct

Explanation:

just got it right on a quiz

The correct option is C, The most important characteristic to look for when trying to identify a lowered portion of the rain-free cloud base as a wall cloud is a persistent rotation.

Rotation refers to the act or process of turning or spinning around an axis or center point. It is a fundamental concept in physics and geometry, describing the circular or angular movement of an object or system.

Rotation is also a key concept in geometry, where it describes the transformation of a shape around a fixed point. When a figure rotates, every point on it moves along a circular path, maintaining the same distance from the center of rotation. The degree of rotation is measured in terms of angles, typically in degrees or radians.

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Like most of the British Isles, Birmingham has a temperate maritime climate (Köppen classification Cfb), with average maximum temperatures in summer (July) of about 21.3 °C (70.3 °F) and in winter (January) of about 6.7 °C (44.1 °F). It is mainly cloudy.

Showers are likely in the afternoon after a slight chance of showers in the morning. a high of about 60. In the afternoon, the temperature will drop into the mid-50s. Lower 90s are the typical afternoon high temperatures. On 70 to 80 days, readings of 90 or higher should be anticipated. Typically, overnight lows fall between the upper 60s and lower 70s. The winter months have more fluctuating temperatures.

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Answer:True

Explanation: Definition of erosion

The statement "erosion is the breakdown of rock and mineral at the earth's surface" is true because erosion is a natural process that occurs when physical and chemical forces wear down and remove rock and soil from the earth's surface.

This can happen due to a variety of factors, including wind, water, ice, and gravity. Water erosion is perhaps the most common type of erosion, and occurs when rainfall or flowing water wears away soil and rock, carving out valleys, canyons, and other features. Wind erosion occurs in arid regions where strong winds blow sand and dust, creating dunes and other formations. Glacial erosion occurs when glaciers scrape and grind against rock, carving out valleys and shaping the landscape.

Erosion can have both positive and negative effects on the environment. On one hand, erosion can create new landscapes and habitats, and can help to fertilize soil by depositing mineral-rich sediments. On the other hand, erosion can also cause soil degradation, desertification, and other environmental problems. Overall, it is important to understand the causes and effects of erosion in order to mitigate its negative impacts and preserve our planet's natural resources.

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Answer:

Thermometer

Explanation:

A thermometer measures the temperature, which is either written in Celsius (C) or Fahrenheit (F)

Answer:thermometer

Explanation:

I just took the test and I got it right also this question is super easy

Answer:

Drake Passage

I hope this helps

Answer:

30. atacama desert

34. Andes mountains

27. llanos

Explanation:

In the northern Hemisphere, air tends to rotate clockwise around and converge toward low pressure systems when friction, the pressure gradient, and Coriolis forces act on it.

The Coriolis force is a consequence of the Earth's rotation and acts to deflect moving objects to the right in the northern Hemisphere and to the left in the southern Hemisphere. When air is forced to move from high to low pressure areas, this force causes the air to rotate around the area of low pressure in a clockwise direction. This is known as cyclonic rotation.

The pressure gradient force is the difference in atmospheric pressure between the high and low pressure systems. This force acts to move the air from high to low pressure areas and it is the main driver for winds. On the other hand, friction acts in the opposite direction of the wind and slows down the air flow. As the air moves from high to low pressure, these three forces interact with each other to cause the air to rotate and converge toward the low pressure area.

Together, the combined action of these forces causes air to rotate clockwise around and converge toward low pressure systems in the northern Hemisphere.

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The Coriolis force and latent heat play crucial roles in the development and intensification of tropical cyclones. Here's an explanation of their impacts:

Coriolis Force:

The Coriolis force is an apparent force that deflects moving objects, including air masses, due to the rotation of the Earth. In the context of tropical cyclones, the Coriolis force influences cyclonic circulation and helps in their formation and organization. Its impact can be summarized as follows:

Formation: The Coriolis force is essential for initiating the rotation of air around a low-pressure system, which is a necessary condition for tropical cyclone formation.

Cyclonic Circulation: The Coriolis force contributes to the cyclonic circulation pattern of a tropical cyclone. As the air converges towards the low-pressure center, the Coriolis force causes it to rotate around the center in a cyclonic (counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere) fashion.

Spiral Bands: The Coriolis force also influences the formation of spiral rainbands around the core of a tropical cyclone. These rainbands are a prominent feature of mature cyclones and are responsible for the distribution of heavy rainfall and gusty winds.

Latent Heat:

Latent heat plays a critical role in fueling the energy of tropical cyclones. When water evaporates from the warm ocean surface, it absorbs heat from the ocean, storing it as latent heat. The release of this latent heat during condensation in the cyclone's cloud systems provides a significant source of energy for intensification. The impact of latent heat can be summarized as follows:

Heat Engine: Tropical cyclones are often referred to as "heat engines" because they rely on the release of latent heat to sustain their energy and intensify. As moist air rises in the cyclone, it cools and condenses, releasing the stored latent heat.

Intensification: The input of latent heat through the condensation process drives the upward motion and rapid development of thunderstorms within the cyclone.

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Answer:

Trenches are not found int he Appalachian mountain province today.

Explanation:

1 is not correct because there is an abundance of metamorphic rocks, which is not weird considering the age of this mountain range.

2 is not correct because this mountain range has been close to intense volcanism during its formation, so it still has some of the volcanic rocks preserved.

3 is not correct because there are a lot of folded and faulted mountain ridges, many of which are visible at the surface today.

4 is not correct because these mountains rose from the ocean, so there are remnants of an ancient floor at places.

5 is not correct because with the erosion over hundreds of millions of years, valleys have been gradually formed at the periphery of this mountain range.

6 is not correct because the top layers of this e range are predominantly made of sedimentary rocks.

7 is correct because the trenches that existed in this area have disappeared a couple of hundreds of millions of years ago, mainly because the area has been gradually moving away from the tectonic boundaries and became an area that is tectonically inactive.

Until 1996, when an amendment to the Education Act raised the school leaving age to 16, most Bahamian children stayed in school until they completed the 12th grade, generally at the age of 17 or 18.

The Bahamas was able to announce to the United Nations that we had accomplished the vast majority of the millennium goals for education, even while these were still being formulated in international circles, with great pleasure.

To identify a rock in the field to see whether they are igneous, sedimentary, or metamorphic, you must first inspect its texture and mineral composition. Igneous rocks have a glassy or crystalline texture, and they are formed from magma or lava cooling and solidifying.

Sedimentary rocks are created by the weathering of other rocks, and they can have a clastic texture with fragments or a crystalline texture with calcite, halite, or gypsum.

Metamorphic rocks are made from existing rocks that are subjected to heat, pressure, and chemical processes. They can have a foliated texture, such as slate or gneiss, or a non-foliated texture, such as quartzite or marble.

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Answer:

B. too much water being taken from underground aquifers

Answer:

b on edge

Explanation:

Answer:

A lizard is a vertebrae

Explanation:

"Reptiles are vertebrates that have scales on at least some part of their body, leathery or hard-shelled eggs, and share a number of other features."

The North American interior experiences a continental climate, which is characterized by a lack of significant seasonal variation in temperature range. In this type of climate, the temperature range remains relatively stable throughout the year, resulting in moderate to cold temperatures.

The temperature range in a continental climate is primarily influenced by the large landmass and the distance from large bodies of water. In contrast to coastal regions, which are moderated by the ocean, the interior of North America experiences greater temperature extremes due to its distance from the moderating influence of the ocean. During the winter months, the interior experiences colder temperatures due to the cold air masses that move southward from the polar regions. During the summer months, the interior experiences warm temperatures as warm air masses move northward from the tropics.

However, despite these seasonal temperature fluctuations, the temperature range in the North American interior remains relatively stable throughout the year. This is because the interior is located far from the moderating influence of the ocean, and the large landmass acts as a heat sink, absorbing and retaining heat. This results in a more gradual transition of temperatures, leading to a smaller seasonal variation in temperature range compared to coastal regions.

In conclusion, the North American interior experiences a continental climate, which is characterized by a relatively stable temperature range throughout the year. The temperature range in this region is influenced by the large landmass, distance from large bodies of water, and the movement of air masses.

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Answer:

A. Communist governments have used up all its coal

Explanation:

Answer: b

Explanation:because I got the question right!

Answer:

Away from her push, because the wall exerts a stronger force in the same direction so B for me.

Explanation:

Answer:

257 persons per square km

Explanation:

Given parameters:

Population of the island  = 1394973

Area of the island  = 5131km²

Unknown:

Population density in 2018  = ?

Solution:

The population density of a place is the number of people living per square km in such a place.

  Population density  = \(\frac{number of people}{land area}\)

  Now insert the parameters and solve;

 Population density  = \(\frac{1394973}{5131}\)  = 257 persons per square km

Answer:

it's A I am sure Namibia is closer to it if not then Zimbabwe

Answer:

Chlorofluorocarbons (CFCs) are chemicals that release chlorine and bromine into the atmosphere, which break down the ozone molecules in the ozone layer and cause depletion of the ozone layer.

Chlorofluorocarbons result in the depletion of the ozone layer of the earth.

The Earth's ozone layer shields all life from the sun's damaging radiation, but human actions have harmed it. Less ozone-layer protection from ultraviolet (UV) radiation will eventually harm crops and lead to greater instances of skin cancer and cataracts.

The ozone layer in the stratosphere absorbs some of the sun's radiation, preventing it from reaching the planet's surface. Most notably, it absorbs UVB light. UVB has been associated to a variety of negative outcomes, including skin cancer, cataracts, and crop and marine life damage.

When gaseous CFCs slowly climb into the stratosphere, they are broken down by intense UV light, releasing chlorine atoms, which subsequently combine with ozone molecules.

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