Conclusion/Summary: What is the way forward regarding droughts for the government and the people of South Africa
chronologically speaking, this one was first. (a) alexander the great (b) cyrus the great (c) julius caesar (d) julius ii
Chronologically speaking, Cyrus the Great (b) was first among the options provided.
Here is the order of their reigns:
1. Cyrus the Great (b) - reigned from 559 BC to 530 BC
2. Alexander the Great (a) - reigned from 336 BC to 323 BC
3. Julius Caesar (c) - in power from 49 BC to 44 BC4. Julius II (d) - reigned as Pope from 1503 to 1513 AD
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the nighttime counterpart of the sea breeze circulation is called a
The nighttime counterpart of the sea breeze circulation is called a land breeze.
During the day, the sun heats up the land faster than it heats up the ocean, causing the air above the land to rise and creating an area of low pressure. This draws in cooler air from the ocean, which creates the sea breeze circulation.
At night, the situation is reversed. The land cools faster than the ocean, which causes the air above the land to become cooler and denser, creating an area of high pressure. This draws in warmer air from the ocean, which creates the land breeze circulation. The land breeze typically occurs in the late evening and early morning hours.
Therefore, the land breeze is the nighttime counterpart of the sea breeze circulation, and both are important atmospheric circulations that help to regulate the temperature and weather patterns near coastal regions.
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the cycle of splitting of a supercontinent, opening of an ocean basin, followed by closing of the basin and collision of the continents, is known as a .
A "Wilson Cycle" is a series of events that involves the separation of a supercontinent, the opening of an ocean basin, the closing of the basin, and the collision of the continents.
The Wilson Cycle is named after J. Turo Wilson, a Canadian geophysicist who proposed the idea in the 1960s. It describes the process by which a supercontinent (such as Pangaea) breaks apart and separates into smaller landmasses, which then move away from each other and form new ocean basins. These ocean basins continue to widen as seafloor spreading occurs, until eventually the oceanic crust collides with a continental margin and begins to subduct.
The Wilson Cycle is a geologic concept that describes the formation, evolution, and eventual destruction of ocean basins. It starts with the breakup of a supercontinent due to plate tectonic processes, leading to the formation of a new ocean basin. As the ocean basin expands, new oceanic crust is created at the mid-ocean ridge.
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The telescope at a small observatory has objective and eyepiece focal lengths respectively of 18.8 m and 12 cm. If this telescope is used to view a 1740 m diameter lunar crater on the surface of the moon 3.77 x 108m from the surface of the Earth, determine the following. (a) Angular magnification of the telescope. (b) Size of the first image. (c) Length of the barrel of the telescope. (d) Angle subtended at the unaided eye by the lunar crater. (e) Angle subtended at the eye when the lunar crater is viewed through the telescope.
Te angle subtended at the eye when the lunar crater is viewed through the telescope is 2813.25 degrees.
(a) Angular magnification of the telescope:
The angular magnification of the telescope can be calculated using the formula:
M = fo / fe
Where fo is the focal length of the objective lens and fe is the focal length of the eyepiece.
Substituting the given values, we get:
M = 18.8 m / 0.12 m = 156.67
Therefore, the angular magnification of the telescope is 156.67.
(b) Size of the first image:
The size of the first image formed by the objective lens can be calculated using the formula:
h = Do * θ
Where h is the size of the image, Do is the diameter of the objective lens, and θ is the angular size of the lunar crater.
The angular size of the lunar crater can be calculated as:
Therefore, the size of the first image formed by the objective lens is 0.0867 mm.
(c) Length of the barrel of the telescope:
The length of the barrel of the telescope is the sum of the focal lengths of the objective and eyepiece lenses. Substituting the given values, we get:
Length of the barrel = 18.8 m + 0.12 m = 18.92 m
Therefore, the length of the barrel of the telescope is 18.92 m.
(d) Angle subtended at the unaided eye by the lunar crater:
The angle subtended at the unaided eye by the lunar crater can be calculated as:
θ = 49.21 radians * (180 / π) = 2813.25 degrees
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what amber is and how it formed
silurian and devonian layers are dipping toward the _____. Select one: a. West b. East c. Southeast d. Northeast e. Northwest of South g. North O h. Southwest
The Silurian and Devonian layers are dipping toward the Southeast.
To provide an explanation, let's first understand the terms Silurian and Devonian. The Silurian and Devonian periods are two distinct intervals in Earth's geological history, spanning from about 443 to 358 million years ago. The Silurian period came first, followed by the Devonian period.
These time frames are characterized by the formation of various rock layers or strata, which can be found in different locations worldwide.
The term "dipping" in the context of geology refers to the angle at which rock layers or strata are inclined relative to the horizontal plane. The direction of the dip is the direction towards which the rocks tilt or incline. In this case, we are discussing the dipping direction of Silurian and Devonian layers.
The layers from these periods are known to dip toward the Southeast in some regions, such as parts of the Appalachian Mountains in North America.
This dipping direction is the result of geological processes that have occurred over millions of years, including tectonic plate movements, sediment deposition, and rock deformation. These processes have caused the rock layers to tilt and bend, resulting in their current orientation.
In summary, the Silurian and Devonian layers are dipping toward the Southeast. This orientation is a product of geological events that have taken place over millions of years and can be observed in specific regions globally, such as the Appalachian Mountains.
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The most dangerous threat to the marine environment, overall, is probably:
a. human overpopulation.
b. refined oil spills.
c. solid waste and synthetic pesticides.
d. excessive greenhouse heating.
Answer:
b. refined oil spills
Explanation:
Beacuse If oil spills in sea then marines cant go in ships
The most dangerous threat to the marine environment, overall, is probably excessive greenhouse heating. This is because rising temperatures can cause several problems for marine life. For instance, warming oceans can cause coral bleaching, which happens when coral reefs lose their vibrant colors and turn white.
Coral reefs are home to a vast array of marine species, and their destruction can have significant impacts on the ecosystem. Moreover, rising temperatures can cause an increase in the frequency and intensity of storms, leading to more coastal erosion and habitat destruction.
This can have harmful effects on the shells and skeletons of marine organisms, making it difficult for them to survive and reproduce. Acidification can also affect the food chain, as many species depend on these organisms for survival.
In conclusion, excessive greenhouse heating is the most significant threat to the marine environment, and urgent action is needed to address this problem. We must reduce our greenhouse gas emissions and take steps to mitigate the impacts of climate change on the ocean and its inhabitants.
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Were latitude the only control of temperature, the isotherms would run straight across the maps from east to west. Choose one region of the world where this hypothetical isotherm pattern is actually observed. Group of answer choices
Over the oceans
Over the continents
Over North Africa and the Sahara Desert
Over the oceans, since the water moderates temperature and creates more uniform conditions compared to the fluctuating temperatures over land. Therefore, the isotherms tend to run straight across the maps from east to west in oceanic regions.
However, this scenario is not observed in most regions of the world due to the presence of other factors that affect temperature variations, such as ocean currents, altitude, prevailing winds, and vegetation cover. As a result, the isotherms in different regions of the world follow complex patterns that reflect the interplay of these factors.
That said, the isotherms in oceanic regions tend to follow the hypothetical pattern mentioned above, running straight across the maps from east to west. This is because the large water bodies, such as oceans and seas, act as heat sinks that absorb and release heat more slowly than land surfaces. As a result, the temperature over oceans tends to be more uniform, with smaller variations between different latitudes. This creates a pattern of isotherms that are relatively straight, with a gradual decrease in temperature as one moves away from the equator towards the poles.
In contrast, over the continents, the temperature variations are much more pronounced due to the absence of large water bodies that can moderate the temperature. This leads to a more complex pattern of isotherms, which are influenced by factors such as altitude, prevailing winds, vegetation cover, and ocean currents in nearby regions.
Therefore, while the hypothetical pattern of isotherms running straight across the maps from east to west is not observed in most regions of the world, it is a characteristic feature of oceanic regions where large water bodies act as heat sinks to moderate temperature variations.
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which is correct sequence of metamorphic change? choose one:a. shale, slate, phyllite, schist b. phyllite, shale, slate, schist c. slate, schist, phyllite, shale d. shale, phyllite, slate, schist
a. shale, slate, phyllite, schist
This is known as the regional metamorphic sequence, where shale undergoes increasing levels of pressure and temperature to form slate, then phyllite, and finally schist.
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Of the following statements about the Ekman spiral and Ekman transport, which is/are true? Choose all that apply.
- Ekman transport is to the right of the wind direction in the Northern Hemisphere.
- The Coriolis effect causes surface waters to move at an angle relative to the wind direction.
- Ekman transport can result in both upwelling and downwelling. In the deeper layers of the Ekman spiral, water can move in a direction opposite of the wind direction.
In the deeper layers of the Ekman spiral, water can move in a direction opposite of the wind direction due to the complex interactions between the Coriolis effect and friction.
All three statements are true. The Ekman spiral describes the pattern of water movement caused by the Coriolis effect and friction between the wind and water. Ekman transport refers to the net movement of water perpendicular to the wind direction, which is to the right of the wind direction in the Northern Hemisphere due to the Coriolis effect. This transport can result in both upwelling and downwelling, which can have important impacts on ocean productivity and climate. In the deeper layers of the Ekman spiral, water can move in a direction opposite of the wind direction due to the complex interactions between the Coriolis effect and friction.
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If the sediments in the rockfall deposit were lithified together as they currently rest, without any further movement downslope, what kind of sedimentary rock would they form?
A. limestone
B. granite
C. sandstone
D. breccia
E. conglomerate
The answer is E. conglomerate. Conglomerate is a sedimentary rock that is formed when sedimentary particles (such as gravel, cobbles, and boulders) are lithified together.
What is conglomerate?Conglomerate is a business structure in which a company is made up of a number of different, unrelated businesses. These businesses typically have nothing to do with each other and may even be in competing industries. A conglomerate is typically owned by a large parent company that owns and manages the individual businesses. The purpose of conglomerates is to diversify, allowing the parent company to reduce its risk and increase its profits.
In this case, the rockfall deposit consists of these sedimentary particles, so if it were lithified together without any further movement downslope, it would form a conglomerate sedimentary rock.
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how much more intense is an earthquake of 8.6 magnitude compared to an earthquake of 4.5 magnitude? show all your work.
An earthquake of 8.6 magnitude is significantly more intense than an earthquake of 4.5 magnitude. In fact, it is about 31,623 times stronger in terms of energy released.
The Richter scale is logarithmic, which means that each whole number increase in magnitude represents a tenfold increase in amplitude and about a 32-fold increase in energy released.
Therefore, an earthquake of magnitude 8.6 has 1000 times greater amplitude than an earthquake of magnitude 4.5, and releases approximately 1000 × 1000 × 32 = 31,623 times more energy.
The Richter scale is used to measure the magnitude of earthquakes. It is a logarithmic scale that assigns a numerical value to the amount of energy released during an earthquake.
For example, an earthquake with a magnitude of 6.0 is 10 times more powerful than one with a magnitude of 5.0, and 100 times more powerful than one with a magnitude of 4.0. The scale ranges from 0 to 10, but in practice, earthquakes with a magnitude of 7.0 or higher are considered major earthquakes, and those with a magnitude of 8.0 or higher are considered great earthquakes.
The Richter scale is used by seismologists to report earthquake magnitudes and to assess the potential impact of an earthquake.
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23. If a parcel of air has a RH of 50% and a water vapor content of 7 g/kg, what is its temperature? 24. At what point during the day would you expect outside relative humidity values to be the lowest? Highest? Explain your reasoning 25. During which of these two days does the air have a greater volume of water vapor? Show your work and justify your answer Day 1: Air Temperature. 86°F and RH 60% Day 2: Air Temperature: 41°F and RH-90% 26. Considering your answers for 1125, does a higher percentage for Relative Humidity always mean that there is more water vapor in the air? Explain
Answer:
Explanation:would a parcel of air at 35oc with a water vapor content of 17.5 g kg be saturated or unsaturated?
Would a parcel of air at 35 degrees C with a water vapor content of 17.5 g/kg be saturated or unsaturated? Explain your answer. Unsaturated. It would take water vapor content of 20 g/kg to saturate the air Unsaturated.
The lowest and highest outside relative humidity values would depend on various factors such as the time of day, temperature, and local weather conditions.
In general, relative humidity tends to be lowest during the warmest parts of the day when the air can hold more moisture, and highest during the cooler parts of the day or during periods of high moisture content in the air, such as during or after rainfall.
For question 26, a higher relative humidity does not necessarily mean that there is more water vapor in the air. The amount of water vapor that air can hold depends on its temperature and pressure, so a higher relative humidity may indicate that the air is nearing its saturation point, but not necessarily that there is more water vapor present.
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cloudy, rainy conditions would accompany a ____________ pressure area.
Answer:
Cloudy, rainy conditions would accompany a low pressure area.
Enter Mercury's orbital period to confirm that the Calculator returns the planet's a value. Which of the following best describes the calculations you have performed? There is not enough information to choose. The closer a planet is to our Sun, the slower it travels along its orbit. O All planets travel at the same speed along their respective orbits. The closer a planet is to our Sun, the faster it travels along its orbit.
Mercury's orbital period is approximately 88 Earth days. This means it takes 88 days for Mercury to complete one orbit around the Sun.
The question is asking about the orbital period of Mercury, which is the time it takes for Mercury to complete one orbit around the Sun. The calculation performed is to enter this value into a calculator to confirm that it returns the correct result. The correct answer to the multiple-choice question is "The closer a planet is to our Sun, the faster it travels along its orbit." This is because the closer a planet is to the Sun, the stronger the gravitational pull is, which causes the planet to travel faster in its orbit around the Sun.
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Summarize the three winter holidays of Three Kings Day, Kwanzaa, and Hanukkah. Explain why these holidays are honored and how they are celebrated by individual cultural groups.
what type of amphibole is mentioned in this narration? group of answer choices augite hornblende grunerite no answer text provided.
In the provided narration, there isn't enough information to determine the specific type of amphibole mentioned. Please provide more context or details to accurately identify the amphibole as augite, hornblende, or grunerite.
Amphibole is a group of rock-forming minerals characterized by their long, thin crystals and prismatic shape. These minerals are commonly found in igneous and metamorphic rocks, as well as in some sedimentary rocks. Amphiboles are composed of complex silicate chains that give them their characteristic structure and physical properties. They typically have a dark color and a high density, and can exhibit a wide range of chemical compositions. Amphiboles are important in geology because they provide clues about the conditions under which rocks were formed, and can also be used as indicators of the temperature and pressure of the Earth's interior.
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Wallace Creek is an ephemeral stream that is dry most of the time but flows during the wet seasons. Flow is from the North American side toward the Pacific side. Points a, b, and c on the Pacific Plate side mark points where Wallace Creek has flowed across the fault at various times in the past from point d on the North American side. Geologists interpreted the approximate ages of initial development of the Wallace Creek channels as follows: (see Figure above).
a = 13,000 yrs
b = 10,000 yrs
c = 3,700 yrs
1. What is the general direction of displacement (movement) of the Pacific Plate side of the fault?
N
NE
E
SE
S
SW
W
NW
2. What is the average velocity (cm/yr) of displacement on this fault in the last 13,000 yrs? Provide your answer in cm/yr.
The Pacific and North American tectonic plates are separated by the more than 700 miles (1100 kilometres) long San Andreas fault.
What is a good example of Wallace Creek?Wallace Creek used to drain directly across the fault, but the San Andreas Fault's movement has changed the drainage path, with the downstream part now being about 430 feet northwest of the upstream segment. One of the world's best instances of stream offset across a fault can be seen here.
Which two sections of Wallace Creek were in motion?Previously, the watercourse traveled directly from the North American Plate to the Pacific Plate. The Pacific Plate portion of Wallace Creek, however, moved northwest of the North American Plate as the North American Plate shifted to the southeast and the Pacific Plate to the northwest.
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Pls help me construct a multiple line graph thank u
If you're looking to create a multiple line graph, simply follow the steps below:
The StepsFirstly, choose the data sets you want to plot. Analyze each of these datasets and determine how they should be represented on the graph. Afterwards, construct a table with the data that must be illustrated; with each row exhibiting a designated timeframe/category and every column symbolizing an individual dataset.
Subsequently, select a graphing software - Excel, G o o g le Sheets, or R are all popularly used alternatives - that can fabricate s uch charts. Next, input the data from the previously composed table into this chosen system, picking 'multiple line graph' as the chart type.
Once the fundamental inputs have been established, personalize and beautify the graph; incorporating titles, labels, and styling to your liking. After verifying the correctness of the graph and making any required amendments, finalize it by saving it as an image or shipping it off as a distinguishable file.
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6. If you were uncertain of the type of contact between the granite and the overlying fractured sandstone, which principle would allow you to determine it's nature? a. law of superposition. b. law of original continuity. C. law of original horizontality d. principle of inclusion e.faunal succession
The principle that would allow you to determine the nature of contact between the granite and the overlying fractured sandstone is the principle of inclusion.
So, the correct answer is D.
What's the principle of inclusion?This principle states that any rock fragments included in another rock layer must be older than the layer they are included in.
By examining the type and age of the inclusions in the overlying sandstone, you can determine the nature of the contact between the two rock types.
The other principles, such as the law of superposition, original continuity, original horizontality, and faunal succession, may provide additional information about the sequence and relative ages of the rocks, but they would not specifically help determine the nature of the contact between the granite and sandstone.
For this question the answer is D. principle of inclusion.
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explain the three possible strength types of rock (isotropic, transversely anisotropic and orthotropic), and give an example (rock name) of each one.
Rocks can have different strengths depending on their internal structure and the type of forces they are subjected to. The three possible strength types of rock are isotropic, transversely anisotropic, and orthotropic.
Examples:
Isotropic - granite and marble
Transversely anisotropic - shales and some sandstones
Orthotropic - slate and schist
Isotropic: An isotropic rock has the same mechanical properties in all directions. This means that it has the same strength and stiffness in all directions. Examples of isotropic rocks are granite and marble.
Transversely anisotropic: A transversely anisotropic rock has different mechanical properties in two perpendicular directions, but it is the same in the third direction. This means that it has different strengths and stiffnesses in the horizontal and vertical directions, but the same in the depth direction. Examples of transversely anisotropic rocks are shales and some sandstones.
Orthotropic: An orthotropic rock has different mechanical properties in three perpendicular directions. This means that it has different strengths and stiffnesses in the horizontal, vertical, and depth directions. Examples of orthotropic rocks are foliated rocks such as slate and schist.
It's important to note that different rocks can have varying levels of anisotropy or isotropy. The above examples are just general classifications based on the degree of symmetry in their internal structure.
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1. What do variations in the mineralogy and textures of metamorphic rocks tell us?
A The age of the rock
B The distance the grains have travelled
C When metamorphism occurred
D The degree or grade of metamorphism
a soil sample was taken at the middle of the clay layer and a consolidation test was draw the vertical stress profile
Based on the information provided, a soil sample was taken at the middle of the clay layer and a consolidation test was conducted to draw the vertical stress profile.
The results of the test would indicate how the clay layer responds to loading over time. This information is important for engineering purposes, as it can help determine the settlement characteristics and stability of structures built on or near the clay layer.
The vertical stress profile would show the change in stress with depth, with higher stress levels closer to the surface and lower stress levels deeper in the clay layer. Understanding these stress levels is crucial in designing structures that can withstand the loads imposed by the soil.
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A soil profile at a site is shown in Figure 1. A soil specimen is taken from the middle of the clay layer and subjected to a consolidation test, and following properties are reported.
• Moisture content of clay = 20%
• Specific gravity of soil grains = 2.7 • OCR=2.0
• Compression Index (Cc)=0.3
• Recompression Index (Cr)=0.03
a) Calculate the effective vertical stress at the middle of the clay layer
b) Calculatethepre-consolidationpressure
c) A building foundation will increase the vertical effective at the middle of the claylayer by 57kPa. Calculate the primary consolidation settlement due to the building load.γsat=20.4kN/m3 ClayBedrock height=2.0mWater table Ground Level
Construct a visual grammar that will describe some process of your choice(some simple algorithm, workflow at a production facility, recipe, etc.).Which Gestalt laws can be used to interpret figures that make use of thegrammar?
To construct a visual grammar for a simple algorithm, let's take the example of a workflow in a coffee shop. We'll use various shapes and arrows to represent steps in the process, and then apply Gestalt laws to interpret the figures in this context.
To construct visual grammar, it is important to first choose a process that can be effectively communicated through a series of visual elements. For example, a simple algorithm can be represented through flowcharts, while a recipe can be presented through a series of steps with accompanying illustrations.
Once the process has been chosen, the next step is to identify the key elements and steps involved in the process and determine the best way to represent them visually. This may involve using symbols, diagrams, or other visual aids to clearly convey each step in the process.
To interpret figures that make use of visual grammar, it is important to understand the Gestalt laws of perception. These laws describe how our brains organize visual information into meaningful patterns and structures. Some of the key Gestalt laws that can be applied to interpret figures in a visual grammar include:
1. Figure-ground: This law refers to the way our brains differentiate between the main elements of a visual scene and the background. In visual grammar, this might involve using contrasting colors or shapes to make the key elements stand out from the background.
2. Similarity: This law describes how our brains group together elements that are similar in shape, color, or texture. In visual grammar, this might involve using consistent symbols or visual elements to represent similar steps or processes.
3. Closure: This law refers to our tendency to perceive incomplete visual elements as complete shapes. In visual grammar, this might involve using visual cues or arrows to show the flow of a process from one step to the next.
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Which way was the current (either wind or water) moving during deposition of this section of rocks?
a. towards the left
b. towards the camera
c. towards the right
d. away from the camera
The Current (either wind or water) moves during the deposition of this section of rocks-. towards the left.
Option A is correct
If the rocks are sedimentary, they may have been deposited in a particular environment, such as a river or ocean, and may exhibit sedimentary structures such as cross-bedding or ripple marks that can provide clues about the direction of the current (either wind or water) during deposition.
If the rocks are igneous or metamorphic, they would have formed from the cooling and solidification of magma or the transformation of existing rocks under high temperature and pressure, respectively. In this case, it would not be possible to determine the direction of any current as it does not apply to the formation process of these types of rocks.
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The current moving during deposition of this section of rocks was towards the left. So, option A is accurate.
In the course of the geological process of rock deposition, silt, minerals, or organic particles settle and build up to create sedimentary rocks. Deposition is the process of settling particles that have been carried by water, wind, or ice in a range of environments, such as rivers, lakes, seas, and on land.
Sedimentary particles are moved by wind or water during deposition and eventually land on a surface. Layers of sediment can build up over time, and as new layers are added, the weight of the atop material compresses the underneath sediment, eventually forcing the lower layers to form into rock. Lithification is the term for this procedure.
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in your opinion, do you think the term dark ages is an appropriate label for the period between 200 and 850 ad in europe? why or why not?
Answer: Dark Ages usually refers to the 900 years of European history between the 5th and 14th centuries.
Explanation:
This was a time in history that fell between the end of the Roman Empire and the modern format of European lands. It was also a time period filled with famine, plague or the Black Death, and war, such as the Crusades. The Middle Ages ended with the start of the 14th century and the Renaissance time period
The mistaken notion that the archaeological record is some perfect is:_________
Answer:
Explanation:
The mistaken notion that the archaeological record is some perfect is an illusion.
PLS MARK ME BRAINLIEST
The mistaken notion that the archaeological record is some perfect representation of the past is a fallacy.
The idea that the archaeological record is a perfect representation of the past is a fallacy known as the "Pompeii Premise". This concept is based on the belief that archaeological sites provide a complete and unambiguous picture of past cultures and events. However, the archaeological record is inherently biased and fragmentary, and it is subject to various influences that can distort our understanding of the past.
First, the archaeological record is biased because it only represents a small fraction of past societies. Archaeologists must rely on what has survived, which can vary widely depending on the context and time period. For example, we may have more evidence of elite activities and culture because these individuals had greater access to resources that could preserve their materials over time. This means that the archaeological record may be skewed towards the activities of the wealthy and powerful, rather than the majority of the population.
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if a mineral contained 2000 atoms of a parent isotope when it formed, how many atoms of the parent isotope will remain after 2 half-lives have elapsed?
After 2 half-lives have elapsed, the number of atoms of the parent isotope remaining after 2 half-lives have elapsed is 500.
How to find the number of atoms remaining ?Each half-life represents a 50% reduction in the number of parent isotopes. Therefore, after the first half-life, there will be 1000 parent isotopes remaining (50% of the original 2000).
After the second half-life, there will be 500 parent isotopes remaining (50% of the remaining 1000).
So, the number of atoms of the parent isotope remaining after 2 half-lives have elapsed is 500.
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According to this plot, growth rate and doubling time are
inversely proportional.
directly proportional.
equally proportional to one another.
not related to one another.
The answer is inversely proportional, which means that as growth rate increases, so does
What is rule of 70 ?The "rule of 70" explains a significant relation between the percentage growth rate and its doubling time: divide the number 70 by the percentage growth rate to approximate the doubling time for a steadily growing quantity. The time required for an exponential rate growing population to double is referred to as the doubling time. The fact that the society will always take the same time frame to double no matter when you start measuring is implicit in this definition.
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