T/f - Both Conglomerates (rounded Particles) And Breccias (angular Particles) Are Well-sorted Detrital (2024)

Geography High School

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Answer 1

The statement "Both conglomerates (rounded particles) and breccias (angular particles) are well-sorted detrital sedimentary rocks" is false.

A sedimentary rock is a type of rock that is formed from the accumulation and lithification of sediment. The sediments that make up these rocks are transported by various agents like wind, water, or ice. The process of forming a sedimentary rock involves deposition, burial, compaction, and cementation.Well-sorted sedimentary rocks are those in which the particles are the same size and are uniformly distributed. Conglomerates are sedimentary rocks that consist of rounded particles that are greater than 2 millimeters in diameter. Conglomerates are poorly sorted rocks because they contain a mixture of particle sizes and are not uniform in size.

Breccias are sedimentary rocks that are composed of angular fragments of rock that are cemented together. These angular fragments can be up to several meters in size. Breccias are also poorly sorted because they contain particles of different sizes.

Therefore, both conglomerates and breccias are poorly sorted detrital sedimentary rocks. A concise answer to the question is: False. Both conglomerates (rounded particles) and breccias (angular particles) are poorly sorted detrital sedimentary rocks.

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Related Questions

in the 8 rock samples that you observed, what is the main difference you notice between the extrusive (volcanic) and intrusive igneous rocks? looking at the igneous rock identification table and your samples, what minerals make a rock felsic that are not present in mafic rocks? write 2-4 sentences answering these questions.

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The main difference between extrusive (volcanic) and intrusive igneous rocks is their formation.

Extrusive rocks are formed when magma cools and solidifies on the Earth's surface, resulting in quick cooling and small mineral crystals. In contrast, intrusive rocks are formed when magma cools and solidifies beneath the Earth's surface, allowing for slower cooling and the growth of larger mineral crystals.

In terms of mineral composition, felsic rocks contain minerals such as quartz, feldspar, and muscovite that are not present in mafic rocks. These minerals give felsic rocks their lighter color and lower density compared to mafic rocks, which contain minerals like pyroxene and olivine. The presence of these minerals affects the overall composition and physical properties of the rocks.

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which layer of the earth lies below the crust and extends to a depth of 2900 km?

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The layer below the Earth's crust, extending to a depth of 2,900 kilometers, is known as the mantle. It is composed of solid rock material and plays a significant role in the Earth's internal dynamics through mantle convection.

Below the Earth's crust lies the layer known as the mantle. The mantle extends from the base of the crust to a depth of approximately 2,900 kilometers (1,800 miles). It is one of the major layers of the Earth's interior, located between the crust and the core.

The mantle is primarily composed of solid rock material, rich in silicate minerals such as pyroxenes and olivines. It is divided into two regions: the upper mantle and the lower mantle. The upper mantle is relatively cooler and more rigid, while the lower mantle is hotter and exhibits more plasticity.

The mantle plays a crucial role in the dynamics of the Earth's interior, as it experiences convective movements called mantle convection. This convection is driven by the transfer of heat from the core to the mantle, resulting in the slow movement of the solid rocks over geological timescales.

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a graphical representation of the relationship between the price of a good, service, or resource and the quantities producers are willing and able to supply is known as the supply

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The graphical representation of the relationship between the price of a good, service, or resource and the quantities producers are willing and able to supply is known as the supply curve.

The supply curve represents the quantity of a good that sellers are willing and able to sell at different prices. The law of supply states that as the price of a good increases, the quantity supplied of the good also increases, and as the price of a good decreases, the quantity supplied of the good also decreases.The supply curve is usually upward sloping, which means that the higher the price of a good, the higher the quantity supplied, all other things being equal. This relationship between price and quantity supplied is called the law of supply. The supply curve is used in economics to analyze the behavior of producers in response to changes in market conditions such as price, demand, and input prices.In conclusion, the supply curve is a graphical representation of the relationship between the price of a good, service, or resource and the quantities producers are willing and able to supply. It is an essential tool in understanding the behavior of producers in response to changes in market conditions and is used extensively in the field of economics.

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In the context of data patterns in a time series, a(n) _____ is a one-time variation that is explainable.a.random variationb.seasonal variationc.cyclical variationd.irregular variation

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In the context of data patterns in a time series, a(n) irregular variation is a one-time variation that is explainable. Irregular variation refers to unexpected or unusual changes in data that cannot be attributed to any specific pattern or trend. Option D.

These variations are random occurrences and can be caused by factors such as outliers, errors in data collection, or one-time events that are not expected to repeat in the future.

For example, let's say you are analyzing the sales data of a company over several months. During one particular month, there is a sudden spike in sales due to a special promotion or a major event. This spike in sales would be considered an irregular variation because it is a one-time occurrence that can be explained by the unique circ*mstances of that month.

It is important to note that irregular variations are distinct from other types of variations in a time series. Seasonal variation refers to regular, predictable patterns that occur at specific times of the year, such as increased sales during the holiday season.

Cyclical variation refers to longer-term patterns that repeat over several years, such as economic cycles. Random variation refers to small fluctuations that occur due to random factors and do not follow any specific pattern.

In summary, an irregular variation in a time series data refers to a one-time variation that can be explained by unique circ*mstances or events. It is important to identify and understand these variations to accurately analyze and interpret the data.

Hence, In the context of data patterns in a time series, a(n) irregular variation is a one-time variation that is explainable. Option D.

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A seismological station is located at (0,-3),3km wway from a straight shoreline where the x-axis runs through. The epicentor of an earthquake was determined to be 6km away from the station. If further

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A seismological station is located at (0,-3),3km away from a straight shoreline where the x-axis runs through. The epicentor of an earthquake was determined to be 6km away from the station.

Let point A be the location of the station, and let the epicenter of the earthquake be E. Draw a line segment AE such that AE is 6 km long.Let B be the intersection of AE with the x-axis. Using the Pythagorean Theorem, we can determine that the distance between A and B is [tex]sqrt(6^2 - 3^2) = 3*sqrt(3) km.[/tex]

The point C on the shoreline that is farthest from the epicenter of the earthquake is the reflection of E across the x-axis. Therefore, point C is (6, 3).The distance between the epicenter of the earthquake and the farthest point of the shoreline is the length of segment EC, which is equal to [tex]sqrt((6 - 0)^2 + (3 - (-3))^2) = 2sqrt(30) km.[/tex]

Therefore, the distance between the epicenter of the earthquake and the furthermost point of the earthquake on the surface of the shoreline is 2sqrt(30) km. This can be verified by graphing the points and measuring the distance. Hence, the correct option is 2sqrt(30) km.

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Full question is A seismological station is located at (0,-3), 3km away from a straight shoreline where the x-axis runs through. The epicenter of an earthquake was determined to be 6km away from the station. If the furthermost point of the earthquake is located on the surface of the shoreline, how far was it from the epicenter of the earthquake?

A diurnal tide has __________ high and low tide(s) each day, whereas a semidiurnal tide has __________ high and low tide(s) each day.

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A diurnal tide has one high and one low tide each day, whereas a semi diurnal tide has two high and two low tides each day.

What is a diurnal tide?Diurnal tides are tides that occur once a day. In a diurnal tide, there is only one high and one low tide. Diurnal tides are most commonly found in the Pacific Ocean.What is a semi diurnal tide?Semi diurnal tides are tides that occur twice a day. A semi diurnal tide has two high and two low tides each day. Semi diurnal tides are most common in the Atlantic Ocean.A diurnal tide has one high and one low tide each day, whereas a semi diurnal tide has two high and two low tides each day.

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one reason for the slow response in helping hurricane katrina victims was an antiquated fema system that was held up by bureaucratic red tape.

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Answer:

Explanation:

One of the lessons learned from Hurricane Katrina was that public officials need to lead in crises by communicating confidence to the public and delivering on promises.

Which progression best describes how water goes from the ocean to a river?

a. evaporation ® precipitation ® evapotranspiration

b. evaporation ® precipitation ® infiltration into the ground

c. evapotranspiration ® runoff ® precipitation

d. evaporation ® precipitation ® runoff

Answers

The progression that best describes how water goes from the ocean to a river is: Evaporation ® Precipitation ® Runoff.

What is Evaporation? Evaporation is the process by which liquid water changes into water vapor. The evaporation process happens due to the heat from the sun that causes the water to evaporate. It also happens when air moves over the surface of water and carries some water vapor with it.What is Precipitation?Precipitation occurs when the air cools and the water vapor condenses to form liquid water or ice. The process of precipitation is how water returns to Earth's surface after evaporation. Precipitation can fall directly back into the ocean or can fall on land.

What is Runoff?
Runoff refers to the flow of water that occurs on the surface of the Earth. This occurs when precipitation that has fallen on land runs over the surface, eventually forming streams, rivers, and other bodies of water. Thus, the correct progression best describes how water goes from the ocean to a river is: Evaporation ® Precipitation ® Runoff.

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Why did the first Chinese cities develop on the North China Plain?

The North China Plain was protected from outside invasion.
The river valleys throughout China were overcrowded with people.
Freshwater rivers supplied wide-open and fertile farmlands.
The Grand Canal was built to connect the North China Plain to other rivers.

Answers

The first Chinese cities develop on the North China Plain is Freshwater rivers supplied wide-open and fertile farmlands. Option C is the correct answer.

The development of the first Chinese cities on the North China Plain was primarily influenced by the availability of wide-open and fertile farmlands, which were supported by freshwater rivers.

The North China Plain is characterized by a flat topography and rich soil, making it highly suitable for agriculture. The region experiences a favorable climate and abundant rainfall, further enhancing its agricultural productivity.

The presence of freshwater rivers, such as the Yellow River (Huang He) and its tributaries, provided a reliable water source for irrigation, facilitating the cultivation of crops.

The fertile farmlands and the ability to support a large agricultural population played a crucial role in the development and growth of early Chinese cities.

While the other options mentioned have their significance in Chinese history, they are not the primary reasons why the first Chinese cities developed on the North China Plain. Option C is the correct answer.

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Why did the first Chinese cities develop on the North China Plain?

The North China Plain was protected from outside invasion.
The river valleys throughout China were overcrowded with people.
Freshwater rivers supplied wide-open and fertile farmlands.
The Grand Canal was built to connect the North China Plain to other rivers.

Answers

The first Chinese cities developed on the North China Plain because: Freshwater rivers supplied wide-open and fertile farmlands.

The first Chinese cities developed on the North China Plain because the freshwater rivers in the region provided abundant water supply and fertile lands for agriculture. This allowed for the cultivation of crops, sustaining a stable food supply and supporting the growth of early settlements and urban centers. The fertile farmlands of the North China Plain were favorable for agricultural activities, leading to the development of early civilizations in the region.

Therefore, the correct option among the given choices is: Freshwater rivers supplied wide-open and fertile farmlands.

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What strategies can anthropologists use to study global interconnections?

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Anthropologists, as scholars who study human societies and cultures, have a variety of methods for investigating global interconnections. Anthropologists use multiple strategies to research global interconnections, such as cultural analysis, ethnography, comparative studies, and collaborative research.


Anthropologists who want to study global interconnections could take a variety of approaches. Cultural analysis is one strategy that anthropologists could use to examine global interconnections. Anthropologists can examine the cultural connections between two or more cultures, and they can use this information to study how those cultures have developed over time.
Ethnography is another useful method for studying global interconnections. Ethnography involves immersing oneself in a particular culture to observe and participate in their daily lives. By doing this, anthropologists can gain a more in-depth understanding of how cultures are interrelated and how they are influenced by one another.
Comparative studies are also valuable to study global interconnections. Anthropologists can compare two or more cultures and highlight similarities and differences to identify common patterns and influences. Collaborative research, which involves working with members of the community being studied, is another useful strategy. Collaborative research can provide anthropologists with a deeper understanding of the cultures they are studying, and it can facilitate more accurate interpretations.
In summary, anthropologists can use a variety of strategies to study global interconnections, including cultural analysis, ethnography, comparative studies, and collaborative research. These approaches provide insight into how different cultures are interrelated and how they influence one another.

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What is paleomagnetism Why is it important?

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Paleomagnetism is the study of Earth's magnetic field as preserved in rocks and sediments. It involves analyzing the magnetic properties recorded in rocks to determine the past behavior and changes of Earth's magnetic field.

This field is generated by the movement of molten iron in Earth's outer core. Paleomagnetism is important because it provides valuable information about the past positions of continents, tectonic plate movements, and geological processes. By studying the magnetic properties of rocks, scientists can reconstruct the Earth's magnetic history, determine the past locations of continents, and understand the processes that have shaped our planet over millions of years.

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Long, narrow islands composed mainly of sand that rise out of coastal waters are called ________ islands

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Long, narrow islands composed mainly of sand that rise out of coastal waters are called "barrier islands."

Barrier islands are long, narrow landforms that run parallel to the coastline and are primarily composed of sand.

They typically form off the coast in shallow waters and are separated from the mainland by bodies of water such as lagoons or estuaries.

These islands are created through a combination of geological processes, including sediment deposition and wave action. Over time, sand and other sediment are deposited along the coastline, forming a long ridge or chain of islands.

The shape and size of barrier islands can vary, ranging from a few hundred meters to several kilometers in length.

Barrier islands play a crucial role in coastal ecosystems. They act as a natural buffer, providing protection from ocean waves and storm surges, thereby helping to maintain the stability of the mainland.

They also serve as habitats for various plant and animal species, including nesting grounds for birds and breeding areas for marine life.

Due to their sandy composition and exposure to coastal dynamics, barrier islands are subject to constant change and erosion.

They are influenced by factors such as sea level rise, storms, and human activities. Efforts to preserve and manage barrier islands often involve strategies to mitigate erosion and maintain their ecological functions.

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the rate or intensity of rainfall, such as given in units of in/h, influences the partitioning of water flow between:

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The rate or intensity of rainfall influences the partitioning of water flow between infiltration and runoff. Infiltration happens when rainwater enters the soil, while runoff occurs when rainwater runs off the surface of the ground without being absorbed by the soil.

The amount of rainfall and the duration of the storm both impact the partitioning of water flow. During a low-intensity storm, water has more time to infiltrate into the soil, and as a result, infiltration rates are higher than runoff rates.In contrast, high-intensity rainfall causes water to flow rapidly over the ground surface as runoff rather than infiltrating into the soil. Runoff rates are higher than infiltration rates during these storms. It is due to the fact that the soil has already reached its infiltration capacity, and any extra rainwater is unable to infiltrate the ground. When rainfall is moderate, the partitioning of water flow between infiltration and runoff is usually equal, implying that infiltration and runoff rates are balanced.

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What are the 3 examples of globalization?.

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The three examples of globalization are:

A) International trade and economic integration

B) Cultural exchange and diffusion

C) Technological advancements and communication networks.

A) International trade and economic integration refers to the increasing interconnectedness of economies through the exchange of goods, services, and capital across national borders. This includes the growth of multinational corporations, global supply chains, and trade agreements.

B) Cultural exchange and diffusion involves the spread of ideas, values, and practices across different cultures. It includes the influence of popular culture, such as music, movies, and fashion, as well as the adoption of cultural norms and traditions from different parts of the world.

C) Technological advancements and communication networks have greatly facilitated globalization. The development of transportation systems, the internet, and digital technologies has made it easier for people to connect and share information globally, leading to the rapid exchange of knowledge, innovation, and ideas.

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in the 3-soils simulation shown in class, the loam soil provided the greatest drought avoidance because:

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In the 3-soils simulation, loam soil provided the greatest drought avoidance. Soil type is a crucial factor in determining a plant's ability to resist drought stress. Loam soil has several physical and chemical characteristics that make it well-suited for drought resistance. Let's take a closer look at each of these features:

Loam soil has several physical and chemical characteristics that make it ideal for drought resistance. These features, combined with its well-balanced composition of sand, silt, and clay particles, make it the most drought-resistant soil type.In a loam soil, water penetrates rapidly into the soil because of its high infiltration rate. The high infiltration rate enables water to move through the soil and reach the plant roots, which minimizes the loss of water due to evaporation or runoff.

In addition to its high infiltration rate, loam soil also has a good water-holding capacity. As a result, even when the soil dries out, it retains enough moisture to support plant growth.The pore spaces in loam soil are well-connected, allowing water to move freely through the soil. This feature aids in the movement of water from the soil surface to the plant roots, where it is needed for growth. As a result, loam soil is well-suited for drought resistance.

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match the resource found in sedimentary rocks with its most common, current societal use.

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Sedimentary rocks are rocks that are made of sediment particles that are deposited and compressed over time. They are classified based on their origin, texture, and composition. Sedimentary rocks are an important resource for many industries.

They are used as a source of construction materials, such as gravel and sand, and as a source of fossil fuels, such as coal and oil. The following are some of the most common uses of sedimentary rocks:

Coal - Coal is a sedimentary rock that forms from the compressed remains of plants that lived millions of years ago. Coal is a fossil fuel that is used to generate electricity and as a source of heat.

Sandstone - Sandstone is a sedimentary rock that is composed of sand-sized grains of minerals, rock fragments, and other materials. Sandstone is used as a source of building materials, such as bricks, and as a source of sand for glassmaking.

Limestone - Limestone is a sedimentary rock that is composed of calcium carbonate. It is used as a source of construction materials, such as cement and concrete, and as a source of agricultural lime.

Shale - Shale is a sedimentary rock that is composed of clay minerals and other minerals. It is used as a source of oil and natural gas.

Gypsum - Gypsum is a sedimentary rock that is composed of calcium sulfate. It is used as a source of building materials, such as drywall, and as a source of fertilizer.

Chert - Chert is a sedimentary rock that is composed of silica. It is used as a source of flint for making tools and weapons.

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Alfred Wegener shook up the science community when he proposed that continents drifted across Earth's surface. Wegener's work displayed a key characteristic of the nature of science-imagination. But science is a blend of creativity and logic, so what might start out as a product of imagination must eventually conform to principles of logical reasoning that support conclusions with solid evidence. Developing hypotheses and putting them to the test of logic are creative but disciplined acts. True False Question 19 Our understanding of Earth's past rests on the nature of scientific inquiry. The scientific method argues that some ideas offer better explanations for natural phenomena than others and that those ideas can be tested over and over with similar results. Therefore, our understanding of rests on empirical (capable of being verified or disproved by observation or experiment) evidence that has withstood the scrutiny of the scientific process. a. Earth's origin b. Earth's age c. Earth's rates of change d. all the previous

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The statement "Developing hypotheses and putting them to the test of logic are creative but disciplined acts" is true in the scientific community. As the scientific process argues that some ideas offer better explanations for natural phenomena than others and that those ideas can be tested over and over with similar results.

Therefore, our understanding of Earth's past rests on empirical evidence that has withstood the scrutiny of the scientific process. The nature of scientific inquiry is critical in our understanding of Earth's past. Science is a blend of creativity and logic, and what starts as a product of imagination must eventually conform to principles of logical reasoning that support conclusions with solid evidence.

Wegener's work displayed a key characteristic of the nature of science-imagination. He proposed that continents drifted across Earth's surface. He used the observation of the coastline of different continents and their fitting together like a jigsaw puzzle. He then used logical reasoning to support his conclusions, using geological and paleontological evidence. In the end, Alfred Wegener’s imaginative hypothesis of continental drift was validated with scientific evidence and became a scientific theory.

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in each of the following pairs, which species will have a greater value for standard entropy? (i) f (g) vs. h2o (g) (ii) h2o2 (l) vs. h2o2 (g)

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The following species will have a greater value for standard entropy:

H₂O(g) > F₂(g)

H₂O₂(g) > H₂O₂(l)

Entropy (S) is a thermodynamic property that determines the degree of randomness or disorder of a system. A standard entropy (S°) is the entropy of one mole of a substance under standard conditions at 298 K and 1 atm pressure. To compare the standard entropies of two different species, we must first consider their molecular structure, phase, and size.

Now let's compare the entropy of the following pairs of species.

(i) The entropy of a substance increases as the size of the substance increases. Fluorine (F₂) is a diatomic molecule, while water (H₂O) is a triatomic molecule. As a result, H₂O(g) will have a greater entropy than F₂(g).

(ii) The entropy of a substance increases as the substance changes from a liquid to a gas. H₂O₂(l) is a liquid, while H₂O₂(g) is a gas. As a result, H₂O₂(g) will have a greater entropy than H₂O₂(l).

In conclusion, the following species will have a greater value for standard entropy:

H₂O(g) > F₂(g) and H₂O₂(g) > H₂O₂(l)

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Relocation diffusion

Involves the actual movement of the original adopters from their point of origin, or hearth, to a new place

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Relocation diffusion refers to the spread of an idea, innovation, or cultural trait through the actual movement of individuals or groups from their original location to a new place.

This process involves the physical migration of the original adopters, also known as pioneers, from their point of origin or hearth to a different geographic area.

An example of relocation diffusion is the spread of the English language. During the colonization period, the British Empire established colonies around the world.

As British settlers moved to new territories, they brought their language with them, leading to the diffusion and adoption of English in those regions. This movement of people resulted in the relocation diffusion of the English language.

Another example is the spread of religious beliefs. When missionaries travel to foreign countries to spread their faith, they are engaging in relocation diffusion.

By physically relocating and living in a new place, they introduce their religious beliefs and practices to the local population, leading to the adoption of the religion in that area.

In summary, relocation diffusion involves the movement of individuals or groups from one location to another, leading to the spread of ideas, innovations, or cultural traits. This process can be observed in the spread of languages, religions, and other aspects of culture.

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Which volcanoes are thought to have been about the same size prior to major eruptions?
a. Three Sisters
b. Mount Mazama and Mount Shasta
c. Mount Mazama and Mount Lassen
d. Mount Mazama and Mount Hood
e. Mount Shasta and Mount St. Helens

Answers

Option b Mount Mazama and Mount Shasta are believed to have had comparable sizes before their respective major eruptions. Mount Mazama collapsed to form Crater Lake, while Mount Shasta remains an active volcano.

Mount Mazama and Mount Shasta (Option b) are thought to have been about the same size prior to major eruptions.

1. Mount Mazama: Prior to its eruption around 7,700 years ago, Mount Mazama in Oregon, USA, was a large stratovolcano with an estimated height of about 12,000 feet. The eruption resulted in the collapse of the volcano's summit, forming a caldera that later became Crater Lake.

2. Mount Shasta: Mount Shasta, located in California, USA, is also a stratovolcano and currently stands at around 14,180 feet. It is believed that prior to its last major eruption, which occurred about 200 years ago, Mount Shasta was of similar size to Mount Mazama.

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Has anyone traveled to the backrooms?

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Answer: Yes

Explanation: I have personally been there myself and it was strangely pleasant. Surprisingly, I actually bumped into an old friend named New Zealand. (he is not literally New Zealand the country, he's a person) He's quite friendly actually, let me know if you ever bump into him he's about yay tall and made entirely of sticks. If you'd like to visit the backrooms I'd recommend going to an evacuated space, preferably at dusk or dawn (most people think you should go at 3 AM but my guess is that they're trying to prevent people from traveling to the backrooms and spreading false information) after you're in the evacuated space you simply wait.

Three pieces of advice I have for your safe travels are:

Wear a watch!!!!

Talk to the people you meet there, they tend to get mad if you don't say hi

and lastly, if you want to get out you should run north (I guess you should also bring a compass, preferably a smaller one because the bigger the compass, the more likely it is to malfunction as the magnetic fields in the backrooms are really screwed up.

in order to be called an organic or o horizon, the soil material of that horizon must contain in excess of:

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An O horizon or organic horizon is a soil layer at the surface of the soil that is highly composed of organic matter (litter). The soil material of that horizon must contain in excess of 20% organic matter in order to be called an organic or O horizon.

The O horizon, also known as the organic horizon, is the uppermost horizon in the soil that consists of the remains of organic matter and litter. This horizon contains more organic matter than any other layer in the soil profile.Organic matter is added to the O horizon by decomposing plant and animal material, excreta, and microorganisms. The O horizon acts as a natural buffer, preventing pollutants from reaching deeper soil layers.

Soil is a naturally occurring mixture of mineral particles, organic matter, water, and air. It is a critical natural resource that supports a variety of life forms on Earth. Soils are created through physical, chemical, and biological processes that occur over a long period of time.Soil is made up of horizons, or layers, that can be distinguished from each other based on their physical, chemical, and biological characteristics. The uppermost soil horizon, known as the O horizon, consists of litter and decomposed organic matter, while the lower soil horizons are made up of mineral particles and weathered rock.

Organic matter is the remains of dead plant and animal material that has been broken down by soil microorganisms. It is an important component of healthy soil and provides nutrients to plants and other soil organisms. Organic matter also helps to improve soil structure and water-holding capacity, reduce soil erosion, and buffer against changes in pH.

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What happens at subduction zones?
Huge earthquakes occur constantly.
Plates slide past one another without creating or destroying lithosphere.
Plate edges move away from one another.
Where plates converge, one plunges into the deeper mantle while the overriding plate experiences volcanic activity and buckling that uplifts tall mountain ranges

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Subduction zones occur where two tectonic plates meet and where one plate moves underneath another plate. Here, the two plates converge, one plunges into the deeper mantle while the overriding plate experiences volcanic activity and buckling that uplifts tall mountain ranges.

The subducting plate begins to melt and can cause earthquakes due to its movement. Subduction zones play an important role in the movement of tectonic plates. The lithosphere consists of the earth's crust and the uppermost part of the mantle. At subduction zones, the plate that is denser and heavier sinks below the less dense plate. The sinking plate begins to melt and can cause earthquakes due to its movement. Volcanic arcs develop on the overriding plate due to the melting of the subducting plate. The volcanic arcs that are formed when the subducting plate begins to melt are responsible for creating many of the world's active volcanoes.

Huge earthquakes are frequent in subduction zones, particularly in the ring of fire. These earthquakes are caused by the sudden movement of the plate as it sinks. The movement of the plates creates stress that builds up over time and can be released suddenly as an earthquake.Subduction zones are important for the formation of new crust, the recycling of old crust, and the movement of tectonic plates. Subduction zones play a critical role in shaping the earth's surface and are an important factor in the geology of the planet.

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- ESIK What causes distinct life zones as you ascend in elevation up a mountain? Changes in Temperature Changes in Albedo Changes in Rock Type Changes in Pressure 02 0.5 After the end of the last ice age, why did the Sierra Nevada mountains in California uplift? (Mark all that apply). when the ice was removed, the mantle and crust rises back normal faulting compressional forces along convergent plates batholith intrusion isostatic rebound 00:56 canvas.pasadena.edu - BIH normal faulting compressional forces along convergent plates batholith intrusion isostatic rebound 03 0.5 What trails must be completed to complete the "Triple Crown of Hiking?" (Mark three). Pacific Crest Trail Appalacian Trail Mountains-to-Sea Trail Continental Divide Trail Catalina Island Trail John Muir Trail 1024 0.5 Match the Letters on the map below becaustain 00:57 canvas.pasadena.edu - [is] 5 0.5 What are some of the danger of climbing Mt. Everest? (Mark all that apply). avalanche danger snow blindness low oxygen content tsunami danger cold exposure D 1006 0.5 Match each tectonic boundary with the landforms and geologic activity that occurs there. 00:57 canvas.pasadena.edu on 7 0.5$ What hiking trail spans the Rocky Mountains? American Discovery Trail Continental Divide Trail Pacific Crest Trail Appalachian Trail Iditarod Trail la 8 0.5 Why do earthquakes occur? (Mark all that apply) When the Earth's crust is under stress rocks respond by faulting Convection currents within the mantle crust interface When the Earth's crust is under stress rocks respond by folding Tectonic activity in Earth's crust driven by endogenic processes

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Distinct life zones form on a mountain because of Changes in Temperature, Changes in Pressure, Changes in Albedo, and Changes in Rock Type. Temperature and pressure decrease with elevation, which changes the plants and animals that can survive, creating different zones on the mountain.

For example, in the montane forest, there is a moderate climate that supports numerous species of trees, shrubs, and other plants.Mountains uplift when there are compressional forces along convergent plates, normal faulting, and isostatic rebound after the removal of ice. The Sierra Nevada mountains in California uplifted after the end of the last ice age due to isostatic rebound and normal faulting.

What hiking trail spans the Rocky Mountains? Continental Divide Trail spans the Rocky Mountains. The Continental Divide Trail (CDT) is one of the most extended hiking trails in the world, extending 3,100 miles along the Rocky Mountains' crest in the United States.

What are some of the dangers of climbing Mount Everest? The dangers of climbing Mount Everest include cold exposure, low oxygen content, and avalanche danger. The height of the mountain causes the air to become thinner as you get higher, making it difficult to breathe. This can cause altitude sickness, which can be life-threatening. Low oxygen content is also a contributing factor to the occurrence of cold exposure. Due to the low temperature, climbers' bodies lose heat more rapidly than they can generate it, which results in hypothermia. Avalanches are another potential risk, with numerous mountaineers being killed by them over the years.

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a zone separating two states in which neither state exercises political control.

Answers

Answer:

This zone is called a frontier.

The Appalachian Mountains are low and small compared to the Rocky Mountains. This is because:
the Appalachians are older than the Rockies
the Appalachians are easier to erode than the Rockies
erosion is more intense in the Appalachians
the Appalachians are younger than the Rockies

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The Appalachian Mountains are smaller and lower compared to the Rocky Mountains because they are older and easier to erode than the Rocky Mountains. The Appalachians Mountains are approximately 480 million years old, while the Rocky Mountains are around 80 million years old.

The Appalachians are the oldest mountain ranges in North America, with much of their rock formation occurring during the Paleozoic Era. As a result, they have been subjected to hundreds of millions of years of weathering and erosion.The Appalachians' sedimentary rock formation allowed the mountain range to be easily eroded by streams and rivers, resulting in its reduced height. Over millions of years, the water has eroded the rocks, causing the mountain range's peaks to wear down and flatten out.

In contrast, the Rockies have mostly granite and volcanic rocks that are resistant to erosion, making them taller and more jagged in appearance. The Rockies were created more recently by the collision of the North American and Pacific plates. Therefore, the Rockies' rocks have not had as much time to erode compared to the Appalachian rocks. As a result, the Rockies have sharper and higher peaks, and they are more extensive than the Appalachians. This is why the Rocky Mountains are more significant and higher than the Appalachian Mountains.

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Fill In The Blank, if you believe that climate change is an environmental problem, _________ theories suggest that you will seek media messages that support that opinion

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Confirmation bias theories suggest that you will seek media messages that support that opinion if you believe that climate change is an environmental problem.

Confirmation bias is a cognitive bias that refers to the tendency of individuals to seek, interpret, and remember information in a way that confirms their pre-existing beliefs or hypotheses.

When it comes to beliefs about climate change, confirmation bias theories suggest that individuals who already view climate change as an environmental problem are more likely to actively seek out and engage with media messages that align with their existing beliefs.

For example, individuals who believe in climate change may be more inclined to watch news channels or read articles that present evidence supporting the reality of climate change and the need for action. They may also be more likely to follow social media accounts or join online communities that share similar views.

This selective exposure to information that confirms their beliefs can reinforce their existing opinions and potentially contribute to a more polarized media landscape.

It is important to note that confirmation bias can apply to individuals across the entire spectrum of beliefs about climate change.

People with opposing views may also exhibit confirmation bias by seeking out media messages that align with their skepticism or denial of climate change.

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which mountain range forms the backbone of the east centrl protion of the korean peninsula

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The Taebaek Mountains form the backbone of the eastern central part of the Korean Peninsula, serving as a natural border between the eastern regions of South Korea and western regions of North Korea. The highest peak in this mountain range is Mount Seorak.

The mountain range that forms the backbone of the eastern central portion of the Korean Peninsula is called the Taebaek Mountains. Here's a step-by-step explanation:

1. The Korean Peninsula is located in East Asia and is divided into North Korea (Democratic People's Republic of Korea) and South Korea (Republic of Korea).

2. The eastern central portion of the Korean Peninsula is dominated by a mountain range known as the Taebaek Mountains.

3. The Taebaek Mountains stretch from north to south for approximately 500 kilometers (310 miles) along the eastern coast of the peninsula.

4. The range acts as a natural border between the eastern region of South Korea and the western region of North Korea.

5. The highest peak in the Taebaek Mountains is Mount Seorak (also known as Seoraksan) with an elevation of 1,708 meters (5,604 feet).

6. The Taebaek Mountains are known for their scenic beauty, diverse flora and fauna, and are a popular destination for hiking and nature enthusiasts.

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reference maps show simple themes of geographic properties, such as political boundaries, roads, and cities. group of answer choices true false

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The statement "reference maps show simple themes of geographic properties, such as political boundaries, roads, and cities" is true because reference maps do indeed show simple themes of geographic properties.

These maps provide information about political boundaries, roads, and cities. Reference maps are designed to provide a general overview of a particular area, and they focus on displaying basic geographic features. For example, a reference map of a country might show the borders of different states, major highways, and the locations of major cities.

These maps are often used for general reference purposes and can be helpful for understanding the layout and features of a specific region. Overall, reference maps are a valuable tool for gaining a basic understanding of the geography of an area.

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T/f - Both Conglomerates (rounded Particles) And Breccias (angular Particles) Are Well-sorted Detrital (2024)

FAQs

Do conglomerate and breccia both have angular shaped grains? ›

Grain shape ranges from angular to rounded. For example, breccia has angular grains and conglomerate has rounded grains. Grains tend to become more rounded as they weather.

Is conglomerate well-sorted? ›

There are two broad types of conglomerates: (1) those whose pebbles are generally of one lithology, well-sorted (i.e., narrow size distribution), and matrix-poor; and (2) those with a heterogeneous pebble lithology, poorly sorted, and with abundant matrix. The degree of sorting indicates the method of deposition.

What is the difference between conglomerate and breccia? ›

Breccias are consolidated rubble; their clasts are angular or subangular. Conglomerates are consolidated gravel whose clasts are subrounded to rounded. Sometimes the term rudite (or rudaceous) is used to collectively refer to both breccias and conglomerates.

Is breccia detrital? ›

Breccias are clastic (detrital) sedimentary rocks composed of angular gravel-size clasts. These rocks commonly form along near-surface faults.

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