Answer:
Precipitation varies greatly, from an average of less than five inches annually over the Great Salt Lake Desert (west of Great Salt Lake), to more than 40 inches in some parts of the Wasatch Mountains. The average annual precipitation in the leading agricultural areas is between 10 to 15 inches, necessitating irrigation for the economic production of most crops. However, the mountains, where winter snows form the chief reservoirs of moisture, are conveniently adjacent to practically all farming areas, and there is usually sufficient water for most land under irrigation. The areas of the State below an elevation of 4,000 feet, all in the southern part, generally receive less than 10 inches of moisture annually.
Northwestern Utah, over and along the mountains, receives appreciably more precipitation in a year than is received at similar elevations over the rest of the State, primarily due to terrain and the direction of normal storm tracks. The bulk of the moisture falling over that area can be attributed to the movement of Pacific storms through the region during the winter and spring months. In summer northwestern Utah is comparatively dry. The eastern portion receives appreciable rain from summer thunderstorms, which are usually associated with moisture-laden air masses from the Gulf of Mexico.
Snowfall is moderately heavy in the mountains, especially over the northern part. This is conducive to a large amount of winter sports activity, including skiing and hunting. While the principal population centers along the base of the mountains receive more snow, as a rule, than many middle and northeastern sections of the United States, a deep snow cover seldom remains long on the ground.
Runoff from melting mountain snow usually reaches a peak in April, May or early June, and sometimes causes flooding along the lower streams. However, damaging floods of this kind are infrequent. Flash floods from summer thunderstorms are more frequent, but they affect only small, local areas.
Explanation:
The following is missing for the question to be complete:
Slow; fast
Large; small
Fast; slow
Small; large
Answer: Fast; slow
Explanation: Fast-twitch muscle fibers cause sharp immediate pain and such contraction occurs, for example, in fast running or as in this case, when the elbow is slammed against the door frame. In other words, these fast-twitch fibers therefore rapidly contract, cause sharp pain due to short-term but high effort or strain.
On the other hand, slow twitch muscle fibers therefore slowly contract. The pain due to the action of these fibers occurs after some prolonged activity where like distance running and endurance is needed. Because these muscle fibers are able to withstand the long-term contractions that are necessary for stabilisation after exertion, as is the case here, the pain is felt throughout the next day.
Answer: guhit
your answer needs to be 20 characters long.
Answer:
He should first try to see WHY people are running away from him and screaming. If there is literally no reason for that, maybe try to talk to those people and tell them what they can change about their actions. If there was a reason for the people running and screaming, then maybe the monster can try to change whatever it is about them that's making the people flee. It's whatever the monster's comfortable with.
Answer:
example of construct validity
Explanation:
Construct validity refers to how accurate a study can measure / provide data about the things it claim in the initial description. From the case above, Tara's study claim that it measure<em> 'how social college students are with friends at lunch compared to at dinner' . </em>
In order to measure this, Tara only use 'duration of eye contact' as an indicator of measure it.
The thing is, Social interaction is done with many type of actions, including spoken communication, skin contact, laughter, opened body language ,etc. Only using eye contact will cut off the people who rely their socialization process on these other actions. Because of this, we can say that this study is lacking in validity.
