Answer:
Explanation:
I can´t see the map. Anyway, I will give you the locations of them for you to place them on the map:
- <u>Great Lakes</u> is located on the central part, and central-east of the border between the United States and Canada, in the Great Plains region.
- <u>Arctic Ocean </u>is located in the northernmost part of the planet. Right above Russia, Canada, and Alaska.
- <u>Mississippi River </u>is located in the Great Plains region, in the central part of the United States, running roughly in a north-south direction.
- <u> Yukon River</u> has a flow beginning in the northwestern part of Canada and continues through the central part of Alaska, cutting Alaska roughly in two similar size parts.
- <u>Atlantic Ocean</u> is located between the east coasts of North America and South America, and the west coasts of Europe and Africa.
- <u>Bering Strait</u> is located between Russia and Alaska.
- <u>Hudson Bay</u> is located in the central part of Canada, large body of water that gets deep into the mainland of the country.
- <u> Pacific Ocean</u> is located between the east coasts of Asia and Australia, and the west coasts of North America and South America.
Full
Next to the moon, planet Venus appears most brightly and visibly to Earth. (Because of Venus’s proximity to the Sun, it gets more intense light). Venus gets closer to Earth than any other planet, presenting the same side at each closest approach at inferior conjunction. Hypothetical Venetians would see Earth as full on the other side of the Sun whenever Venus appear full also on the other side of the Sun.
Answer:
There exits various styles of learning some of them are given below.
Explanation:
- The visual style, kinesthetic, auditory and many more. In physical leaning style, the parts of the body are used like the hand and face gestures, sense of touch, etc.
- The visual style is the most common of them as we refer to pictures, diagrams and hence spatial undressing takes place.
- Active listening taking notes, reviewing your work writing summary and overview of the topics.
- Learning becomes more effective when the learner cuts off other distracting environment and focuses on the context.
A slow change to the earth's surface would be the formation of mountain ranges over millions of years due to the shifting of tectonic plates under the earth. Also, another slow change could be considered erosion or weathering. Two rapid changes could be landslides and earthquakes.
The southwest summer monsoon, a four-month period when massive convective thunderstorms dominate India's weather, is Earth's most productive wet season.[37] A product of southeast trade winds originating from a high-pressure mass centred over the southern Indian Ocean, the monsoonal torrents supply over 80% of India's annual rainfall.[38] Attracted by a low-pressure region centred over South Asia, the mass spawns surface winds that ferry humid air into India from the southwest.[39] These inflows ultimately result from a northward shift of the local jet stream, which itself results from rising summer temperatures over Tibet and the Indian subcontinent. The void left by the jet stream, which switches from a route just south of the Himalayas to one tracking north of Tibet, then attracts warm, humid air.[40]
The main factor behind this shift is the high summer temperature difference between Central Asia and the Indian Ocean.[41] This is accompanied by a seasonal excursion of the normally equatorial intertropical convergence zone (ITCZ), a low-pressure belt of highly unstable weather, northward towards India.[40] This system intensified to its present strength as a result of the Tibetan Plateau's uplift, which accompanied the Eocene–Oligocene transition event, a major episode of global cooling and aridification which occurred 34–49 Ma.[42]
The southwest monsoon arrives in two branches: the Bay of Bengal branch and the Arabian Sea branch. The latter extends towards a low-pressure area over the Thar Desert and is roughly three times stronger than the Bay of Bengal branch. The monsoon typically breaks over Indian territory by around 25 May, when it lashes the Andaman and Nicobar Islands in the Bay of Bengal. It strikes the Indian mainland around 1 June near the Malabar Coast of Kerala.[43] By 9 June, it reaches Mumbai; it appears over Delhi by 29 June. The Bay of Bengal branch, which initially tracks the Coromandal Coast northeast from Cape Comorin to Orissa, swerves to the northwest towards the Indo-Gangetic Plain. The Arabian Sea branch moves northeast towards the Himalayas. By the first week of July, the entire country experiences monsoon rain; on average, South India receives more rainfall than North India. However, Northeast India receives the most precipitation. Monsoon clouds begin retreating from North India by the end of August; it withdraws from Mumbai by 5 October. As India further cools during September, the southwest monsoon weakens. By the end of November, it has left the country.[40]
