Are religious and Scientific appoach necessarily dichotomous.?

What impact did the Aztecs religious beliefs haveon cortess appoach to tenochitlan?

Hernan Cortes used the Aztec religious beliefs to his advantage by exploiting the prophecy of Quetzalcoatl's return, claiming to be the god returning, which helped him gain both allies and create fear among the Aztecs. This approach ultimately played a significant role in the downfall of Tenochtitlan as it caused divisions within the Aztec empire and weakened their resistance against the Spanish conquest.

What is the holistic approach method?

maksud pendekatan " the holistic appoach method" dalam ilmu antropologi

What person best demonstrating the interpretative appoach to social research?

Sofia, who goes beyond making observations and tries to make meaning of certain behaviors in her study

What is the cpt code for external appoach septoplasty?

The CPT code for external approach septoplasty is 30520. This code is used for surgical procedures that involve the correction of a deviated septum through an external incision. It's important to consult the latest coding guidelines or resources to ensure accuracy, as codes may be updated or revised.

Fair weather can usually be expected with the appoach of?

Fair weather can usually be expected with the approach of a high-pressure system. High pressure typically brings clear skies and stable atmospheric conditions, leading to pleasant weather. In contrast, low-pressure systems are often associated with clouds and precipitation. Thus, the presence of high pressure indicates a likelihood of fair weather.

What is the minimum safe distance from a house and an electric transformer 13.8 KV?

The transformer enclosure should isolate the transformer sufficiently from the environment. I believe OSHA specifies 2 feet, 1 inch as the minimum appoach distance to 13.8kV, so I suppose a transformer could be put this close to a building and still be safe. My guess is there are codes in place in your local area that prevent this and specify some greater distance.

Why should you give a structured appoach for interactions?

A structured approach for interactions ensures clarity and consistency, making communication more effective and efficient. It helps in managing expectations, reducing misunderstandings, and fostering a collaborative environment. Additionally, a structured framework can enhance the overall experience for all parties involved by providing a clear pathway for engagement and follow-up. This method ultimately leads to more productive outcomes and stronger relationships.

What is broad form comprehensive home insurance?

The Broad form is the "HO3" also known as the "HOC" and sometimes referred to as "All Risk Coverage. It's the priciest Homeowners policy available but also offers the broadest coverage, hence the name "Broad Form". The major difference in the Broad form (HO3) from the Basic Form (HO1) and the Extended Coverage policy (Form HO2) is the peril language appoach. The HO3 is considered to use an "Exclusive" approach where forms 1 and 2 use the "Inclusive" language approach to covered and non-covered perils.

How do you tell a guy you just met without hurting his feelings that you're in love with someone else?

If you have just met him, chances are he is probably not too deeply involved emotionally, so this is the best time to appoach him with this news. Just sit him down and be honest with him, tell him you are telling him this because you dont want to hurt his feelings later on, and it would be worse then. Good luck. Tough one.. Why did you give signals to him in the first place? If you did lead him on, it was your fault. There's no way not to hurt him, if he likes you. You just have to be honest. For example.. either be straightforward.. Or give him clear signals you're not interested. There is no easy way around it. Just tell him you would be unfair if you continued a relationship because you have feelings for someone else.

How does a longshore change a beach?

longshore currents are common at any beach that is exposed to breaking surf. A longshore current is an ocean current that moves parallel to shore. It is caused by large swells sweeping into the shoreline at an angle and pushing water down the length of the beach in one direction. Longsshore currents usually extend from the shallow waters inside the breaking waves to breaking waves on the outside. They vary depending on the size, strength, and direction of the approaching swell, and the length of the beach. The more prominent the swell size and direction, and the longer and straighter the beach is, the more powerful and swift the long-shore current will be. They are responsible for many rescues along the coast by sweeping swimmers and surfers down the beach into a variety of hazards. They also have a large inpact on the shorelineA shoreline is not static. As waves appoach shore and "feel the bottom", water piles up and breakers form (see "Waves"). Primarily these waves, breaking at an angle to the shoreline, are what generate a "longshore current" that parallels the shore. Importantly, the longshore current not only moves water in the surf zone, it also moves sediment parallel to the shoreline. Figure 1 illustrates that the direction of longshore current is a function of the angle of wave appoach. For example, if the waves appoach the shoreline from the south, longshore current moves from south to north.But longshore current and the resulting transport of sediment is only one of the dynamic processes that constantly alter the shoreline. As waves repeatedly hit the shore, water moves onto the beach and then retreats in a continuous cycle. However, the waves are not all that moves on the shoreline. In fact, the sediment on the shore is also always on the move. Great energy is expended on the beach as waves crash against the shoreline. This energy allows the water to transport sediment. The grains are lifted as the waves in the swash zone move onto the beach, and then the grains are deposited again as the water retreats. As long as the waves hit the shoreline "straight on" (i.e., the wave crests are parallel to the shoreline), the sand grains will be picked up and redeposited in the same general area. In this case, no real net movement of sand occurs in the swash zone. However, waves generally do not form parallel to the shoreline, and thus, usually approach the shore at an angle. Consequently, beach sand will have a net movement up or down the beach, depending on the direction of incoming waves. This net movement of the beach sand is known as beach drift.Figure 2 illustrates how beach drift operates. Notice on the diagram the angle at which the waves hit the beach. The water moves onto the beach close to the same angle. Recall that sand grains are transported as the waves move onto the beach. Therefore, the sand grains are being carried in the same direction that the waves are moving. However, when the water retreats, due to gravity it goes straight back perpendicular to the shoreline and not back in the opposite direction from which it came. Since grains are redeposited as the water retreats, the grains are actually deposited further down the beach or down longshore current. Hence, the net overall movement of sand is down current. Also, notice on the diagram that at a given point on the beach, the sediment that has moved down shore is replaced by sediment from further up shore, as long as sediment is available there. The net movement of sediment in Figure 2 is to the south because the waves are hitting the shore from the north. If the waves hit the beach from the south, the net movement of sand will be to the north. Net beach sediment movement, or beach drift, can change back and forth with shifts in wave direction. However, along any particular shoreline one direction for incoming waves usually dominates resulting in a preferential net movement of sediment. Sediment transported by beach drift as well as that moved by longshore current together are called littoral transport.Why are longshore currents dangerous?Long-shore currents can sweep swimmers and surfers into rip currents, piers, jetties, and other hazardous areas. In many cases, the long-shore current is strong enough to prevent swimmers from being able to keep their feet on the bottom, making it difficult to return to shore.

How does a longshore current change beach?

longshore currents are common at any beach that is exposed to breaking surf. A longshore current is an ocean current that moves parallel to shore. It is caused by large swells sweeping into the shoreline at an angle and pushing water down the length of the beach in one direction. Longsshore currents usually extend from the shallow waters inside the breaking waves to breaking waves on the outside. They vary depending on the size, strength, and direction of the approaching swell, and the length of the beach. The more prominent the swell size and direction, and the longer and straighter the beach is, the more powerful and swift the long-shore current will be. They are responsible for many rescues along the coast by sweeping swimmers and surfers down the beach into a variety of hazards. They also have a large inpact on the shorelineA shoreline is not static. As waves appoach shore and "feel the bottom", water piles up and breakers form (see "Waves"). Primarily these waves, breaking at an angle to the shoreline, are what generate a "longshore current" that parallels the shore. Importantly, the longshore current not only moves water in the surf zone, it also moves sediment parallel to the shoreline. Figure 1 illustrates that the direction of longshore current is a function of the angle of wave appoach. For example, if the waves appoach the shoreline from the south, longshore current moves from south to north.But longshore current and the resulting transport of sediment is only one of the dynamic processes that constantly alter the shoreline. As waves repeatedly hit the shore, water moves onto the beach and then retreats in a continuous cycle. However, the waves are not all that moves on the shoreline. In fact, the sediment on the shore is also always on the move. Great energy is expended on the beach as waves crash against the shoreline. This energy allows the water to transport sediment. The grains are lifted as the waves in the swash zone move onto the beach, and then the grains are deposited again as the water retreats. As long as the waves hit the shoreline "straight on" (i.e., the wave crests are parallel to the shoreline), the sand grains will be picked up and redeposited in the same general area. In this case, no real net movement of sand occurs in the swash zone. However, waves generally do not form parallel to the shoreline, and thus, usually approach the shore at an angle. Consequently, beach sand will have a net movement up or down the beach, depending on the direction of incoming waves. This net movement of the beach sand is known as beach drift.Figure 2 illustrates how beach drift operates. Notice on the diagram the angle at which the waves hit the beach. The water moves onto the beach close to the same angle. Recall that sand grains are transported as the waves move onto the beach. Therefore, the sand grains are being carried in the same direction that the waves are moving. However, when the water retreats, due to gravity it goes straight back perpendicular to the shoreline and not back in the opposite direction from which it came. Since grains are redeposited as the water retreats, the grains are actually deposited further down the beach or down longshore current. Hence, the net overall movement of sand is down current. Also, notice on the diagram that at a given point on the beach, the sediment that has moved down shore is replaced by sediment from further up shore, as long as sediment is available there. The net movement of sediment in Figure 2 is to the south because the waves are hitting the shore from the north. If the waves hit the beach from the south, the net movement of sand will be to the north. Net beach sediment movement, or beach drift, can change back and forth with shifts in wave direction. However, along any particular shoreline one direction for incoming waves usually dominates resulting in a preferential net movement of sediment. Sediment transported by beach drift as well as that moved by longshore current together are called littoral transport.Why are longshore currents dangerous?Long-shore currents can sweep swimmers and surfers into rip currents, piers, jetties, and other hazardous areas. In many cases, the long-shore current is strong enough to prevent swimmers from being able to keep their feet on the bottom, making it difficult to return to shore.

How are planes allocated to multiple air traffic controllers at big airports and if a controller is managing a subset of planes how do they avoid conflicts with the planes managed by other controllers?

There are a number of ways aircraft can be allocated to controllers. The simplest would involve allocating particular areas to particular controllers. For example one controller would be responsible for aircraft coming into the airport, another for departing traffic. Another would be a vertical split, one controller for aircraft above a certain level, and lower levels allocated to another. A common division is that between the Approach controller and a Tower controller. The Approach controller would be responsible for an aircraft inbound to the airport, from whenever it is passed from the en-route or area controller, to a point where the aircraft is lined up with a runway for landing. This controller would also be responsible for departing aircraft from just after they get airborne until they reach a particular level or point where they go to the en-route phase of the flight. The tower controller is responsible for the runways, and the immediate vicinity of the airport, so would take inbound traffic from the approach controller, clear it to land, and help get it to the parking stand, and also take departing traffic from the stands to the runway until it is airborne before passing it to the appoach controller. The approach and tower duties may themselves be split up among a number of controllers depending on traffic levels and complexity. To avoid conflicts between adjacent controllers areas of responsibility, all traffic passing from one controller to another must be co-ordinated in some way. This may involve talking directly to the next controller and agreeing a particular level or heading for the aircraft to be on when handed over. Obviously if there is a lot of traffic, this would be hugely time consuming, so there may be some form of written standing agreements. For example it might be agreed that all aircraft will be following a standard published route, and be a a set level before being transferred. Then individual co-ordination would only be necessary in unusual cases where an aircraft cannot meet the requirements, or in a situation where an aircraft is being given priority and individual co-ordination would help to achieve that. i love u all and just to know i m not gay and this isn't my account this is my sister victorias so i just wrote this without permission lol c ya later!!!!!!!!! and also btw i didn't write the rest o this some geek probably did!!!!!!!!!!!!! lol!!!!!