John and Daniel are playing tug-of-war together. John is exerting 10 N of force. Daniel is exerting 12 N of force. What is their net force

The yellow arrows in this illustration represent movement of earth’s tectonic plates.

A tectonic plate (also called lithospheric plate) is a massive, irregularly shaped slab of solid rock, generally composed of both continental and oceanic lithosphere.

Plate size can vary greatly, from a few hundred to thousands of kilometers across; the Pacific and Antarctic Plates are among the largest. Plate thickness also varies greatly,

ranging from less than 15 km for young oceanic lithosphere to about 200 km or more for ancient continental lithosphere (for example, the interior parts of North and South America).

How do these massive slabs of solid rock float despite their tremendous weight? The answer lies in the composition of the rocks.

Continental crust is composed of granitic rocks which are made up of relatively lightweight minerals such as quartz and feldspar. By contrast, oceanic crust is composed of basaltic rocks,

which are much denser and heavier. The variations in plate thickness are nature's way of partly compensating for the imbalance in the weight and density of the two types of crust.

Because continental rocks are much lighter, the crust under the continents is much thicker (as much as 100 km) whereas the crust under the oceans is generally only about 5 km thick.

Like icebergs, only the tips of which are visible above water, continents have deep "roots" to support their elevations.

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Answer:

Cosmic

x-rays

light

heat

radio

Answer:

The answer is A: red fox

Explanation:

Answer:

B. Decrease

Explanation: When an spacecraft is flying away from the moon, the moons gravitational pull on the spacecraft will decrease because gravitational force is directly proportional to the mass of the moon and mass of the spacecraft while inversely proportional to the square of the distance between them. So as the spacecraft moves away from the moon, gravitational pull will decrease.

The 20 or so minerals that predominantly compose Earth's crust are called rock-forming minerals, including silicates like quartz and feldspar, which account for over 90% of the crust.

The approximately 20 or so minerals that make up the bulk of Earth's crust are commonly referred to as rock-forming minerals. Most rocks are composed of these common minerals, and they include silicates such as quartz, feldspar, mica, amphibole, pyroxene, olivine, and various clay minerals. Silicates form over 90 percent of the Earth's crust because the building block of these minerals, the silica tetrahedron, combines one silicon atom with four oxygen atoms.

These rock-forming minerals are significant due to the high abundance of a few key elements in the crust, including oxygen and silicon, which make up about 75% of the Earth's crust by weight. The importance of managing these mineral resources sustainably is also highlighted, as they serve as essential resources for both plant growth and industrial applications.

The basis for dividing the atmosphere into layers is temperature changes with altitude. The correct option is a.

The primary reason for layering the atmosphere is the variation in temperature with height.

Temperature changes occur when we ascend through the atmosphere as a result of a variety of causes, including the absorption of solar radiation, the presence of ozone, and the drop in air pressure.

Within the atmosphere, these temperature variations produce separate areas or layers. The troposphere, stratosphere, mesosphere, thermosphere, and exosphere are among the layers.

The occurrence of particular atmospheric phenomena, temperature profiles, and weather patterns are only a few of the distinctive qualities that each layer has.

As a result, the basic framework for classifying the atmosphere into strata is provided by temperature variations with altitude.

Thus, the correct option is a.

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Your question seems incomplete, the probable complete question is:

what is the basis for dividing the atmosphere into layers

a) Temperature changes with altitude

b) Density changes with altitude

c) Humidity changes with altitude

d) Pressure changes with altitude

Your answer would be C my friend

Friction is a force that opposes motion between surfaces in contact. When an ice skater slides across the ice, friction between the skates and the ice slows them down and eventually brings them to a stop.

Friction is a force that opposes relative motion between surfaces in contact. When an ice skater slides across the ice, friction between the skates and the ice slows down the skater and eventually brings them to a stop. The ice skates exert a force on the ice, and the ice exerts an equal and opposite force on the skates, creating friction.

To keep a sled accelerating downhill, the force of gravity must be greater than the frictional force.

When analyzing the motion of a sled sliding downhill, it's important to understand the forces acting on it and how they contribute to acceleration. Here’s a detailed explanation:

Forces Acting on the Sled

1. Force of Gravity:

  - Gravity: The force of gravity acts vertically downward with a magnitude of ( mg ), where ( m ) is the mass of the sled and ( g ) is the acceleration due to gravity (approximately [tex]\( 9.81 \, \text{m/s}^2 \))[/tex].

  - Component Parallel to the Slope: When the sled is on a slope, only a component of the gravitational force contributes to the sled's motion down the slope. This component is calculated as [tex]\( mg \sin(\theta) \), where \( \theta \)[/tex] is the angle of the slope. This component pulls the sled downhill.

2. Frictional Force:

  - Friction: Friction opposes the motion of the sled. On a slope, this force acts up the slope and is given by [tex]\( f_{\text{friction}} = \mu N \)[/tex], where ( mu ) is the coefficient of friction and ( N ) is the normal force.

  - Normal Force: The normal force is the component of the gravitational force perpendicular to the slope. It is given by [tex]\( N = mg \cos(\theta) \).[/tex]

Conditions for Acceleration

For the sled to accelerate downhill, the net force acting in the direction of the slope must be positive. This requires:

Where:

- [tex]\( F_{\text{gravity parallel}} = mg \sin(\theta) \)[/tex]

- [tex]\( F_{\text{friction}} = \mu mg \cos(\theta) \)[/tex]

Thus:

For the sled to accelerate downhill:

Simplifying this, we get:

In other words, the force of gravity acting parallel to the slope must be greater than the frictional force resisting the motion. If this condition is met, the sled will accelerate downhill. If not, the sled might move at a constant speed or even slide up the slope if the frictional force is greater than or equal to the component of gravity pulling it down.

The life cycles of gymnosperms and angiosperms include seed germination and development stages; however, angiosperms are unique in their production of flowers and fruit-enclosed seeds, which distinguishes them from gymnosperms with exposed seeds on cones.

The life cycles of both non-flowering seed plants, like gymnosperms, and flowering seed plants, known as angiosperms, are characterized by a sequence of developmental stages from seed germination to the production of new seeds. However, there are fundamental differences between these two groups of plants. In the life cycle of a gymnosperm, seeds are not enclosed within a fruit but are often found on the scales of cones. In contrast, angiosperms produce seeds within a fruit, which develops from the flower.

The flower is the reproductive structure that typically includes petals, stamens, pistils, and is responsible for the sexual reproduction of these plants. Angiosperms are divided into two main groups: monocots and dicots. Basal angiosperms differ from other flowering plants in having traits that are more ancestral or less derived. The life cycle of an angiosperm involves alternating generations, with the sporophyte phase being the dominant generation.

The process of seed development in angiosperms is often characterized by the acronym RRAPP, signifying Reduction of the gametophyte, Retention of the gametophyte within the tissues of the parent plant, Arrested development of the seed until favorable conditions, Provisioning of the embryo with nutritive tissue, and Packaging of the seed with a protective coat.

Summarily, the distinctive flower structure and the protected seed development are key differentiators of angiosperms when compared with gymnosperms. Both life cycles show reduction in the haploid stage and growing complexity over time, but angiosperms have advanced further by incorporating flowers and encased seeds into their reproductive strategy.

Answer : The correct option is, (D) Velocity includes rate of change and direction.

Explanation :

Speed : Speed is defined as the distance traveled by an object with respect to the time taken. It is a scalar quantity that means it tell us about the magnitude of an object not direction.

Velocity : Velocity is defined as the rate of change of position of an object with respect to the time. It is a vector quantity that means it tell us about the magnitude and direction of an object.

The only difference between the speed and the velocity is that the velocity tell us about magnitude and direction but speed tell us about magnitude only.

Hence, the correct option is, (D) Velocity includes rate of change and direction.

Speed is a scalar quantity that only considers the magnitude of movement, while velocity is a vector quantity that includes both the magnitude and direction of movement.

D) Velocity includes rate of change and direction.

Speed and velocity are both terms used to describe how fast an object is moving. However, there is a key difference between the two. Speed is a scalar quantity, meaning it only considers the magnitude or size of the movement. Velocity, on the other hand, is a vector quantity. This means it includes both the magnitude and direction of the movement.

For example, if a car is traveling at a speed of 60 miles per hour, that only tells us how fast it is going. However, if we say the car is traveling at a velocity of 60 miles per hour northeast, that tells us both the speed and the direction.

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The law of conservation of energy asserts that energy cannot be created or destroyed, only transformed. This principle applies to eating and exercising by showing that food energy is converted into physical activity and stored fat, highlighting the importance of balancing energy intake with expenditure to manage weight.

The law of conservation of energy states that energy can be neither created nor destroyed, only transferred or transformed from one form to another. In the context of eating and exercising, this principle indicates that the chemical energy from food is converted into various forms such as work (physical activity), thermal energy (heat), and chemical energy stored in body fat. Diets and exercise plans making extraordinary claims should be evaluated for their truthfulness based on this law. If a diet or exercise plan claims to 'destroy' energy or cause weight loss without considering energy intake and expenditure, it is likely not aligned with this fundamental law.

When discussing energy conservation, we can look at our own bodies as energy systems that convert the energy from food into necessary bodily functions and stored energy. If more energy is consumed than what is used for activity and maintaining body temperature, the excess energy is stored as fat. Conversely, if we consume less energy than we use, we tap into these fat reserves to maintain energy balance. Therefore, distinguishing between possible and impossible outcomes when considering exercise and dietary choices becomes clearer under the lens of energy conservation.

To perform a laboratory test of energy conservation, one might set up an experiment to measure the energy input and output in a system to confirm that, despite transformations, the total amount of available energy remains the same. This idea also broadly connects to understanding various forms of energy, such as calories in food, batteries, and heat, illustrating the interconnectedness of physical phenomena.

Answer:

Option (d) is correct.

Explanation:

Speed is defined as the ratio of distance traveled to the time taken.

As distance is scalar quantity, time is also scalar, so the speed is a scalar quantity.

Velocity is defined as the ratio of change in displacement to the time take.

Here displacement is a vector quantity, so velocity is a vector quantity.

So, velocity includes the rate of change of displacement and the direction.

Answer:

[tex]\Huge \boxed{\mathrm{20\ kg \cdot 9.8\ m/s^2}}[/tex]

Explanation:

[tex]\sf Weight \ (N)= mass \ (kg) \times acceleration \ of \ gravity \ (m/s^2)[/tex]

[tex]W=mg[/tex]

The mass of the object is 20 kg.

The acceleration of gravity is approximately 10 m/s².

[tex]W=20 \times 10[/tex]

[tex]W=200[/tex]

The weight of the object is 200 N.