Traditional Culture Encyclopedia - Traditional festivals - What is the difference between like and love? Please help!

What is the difference between like and love? Please help!

How big is the difference between like and love?

The biggest difference lies in the commitment, cognition, and expression of feelings

How big is the difference between liking and loving?

The difference is very, very big, like is a feeling, good is good, bad is bad, love is tolerance, is understanding. Many, many

How big is the difference between humans and animals? Please help

consciousness, but refers to human subjective initiative This question has been raised for many years, but many of the answers that were recognized as correct were eventually shown to be wrong. For example, walking upright, for example, using tools, etc. Subjectivity is not a criterion for distinguishing humans from animals, the world's animals have it too, the problem is that we don't have a precise idea of what subjectivity is, I'm afraid. It is also wrong to say that animals do not have minds, we have not proved this point. It should be said that this seemingly simple question has complex scientific connotations, if you are a student, we suggest that you understand it according to the content of the textbook. Subjective initiative is not possessed by animals. Subjective initiative consists of three aspects: 1. the ability to know the world on the basis of practice and the activity of knowing the world; 2. the ability to transform the world under the guidance of knowledge and the activity of transforming the world; and 3. the state of mind that permeates the activity of knowing and transforming the world. The state of mind that permeates

Is there a difference between loving wrongly and loving wrongly? What is the difference between liking and loving?

Can I understand it like this! When you and a together `think it is love `you both think you are in love `but one day you due to other kinds of reasons separated `or you feel that this is not the love you imagined `when one party to give up the * keep in place of her will have a kind of love wrong feeling! It's also a kind of love for the wrong destiny!

Time and distance are not much different, there is the same **** the same point, is more can change everything, change the original thing, change the original touch

Satisfaction please adopt

The difference between like and love in the end? Please help

The world's largest ocean. It covers an area of 165,250,000 square kilometers (63,800,000 square miles), or about one-third of the Earth's total surface area, and extends from the coast of the Antarctic continent to the Bering Strait, spanning a latitude of 135° and a maximum width of 15,500 kilometers (9,600 miles) from north to south. It extends from the coast of Colombia in South America to the Malay Peninsula in Asia, with a maximum east-west length of 21,300 kilometers (13,235 miles). The average depth (excluding its dependencies) is 4,280 meters (14,050 ft), with a known maximum depth of 11,034 meters (36,200 ft). The northern part is bounded by the Bering Strait, which is only 102 km wide, and the southeastern part communicates with the Atlantic Ocean through the Drake Passage between Tierra del Fuego in South America and Graham Land in Antarctica; the demarcation line between the southwestern part and the Indian Ocean is as follows: from Sumatra to Timor Island via Java Island, and then through the Timor Sea to Cape Londonderry in Australia, and then from the southern part of Australia through the Bass Strait, by the Bass Strait, and then through the Timor Sea to Cape Londonderry in Australia; and then from the southern part of Australia through the Bass Strait, by the Bass Strait, by the Bass Strait, by the Bass Strait. From the south of Australia, through the Bass Strait, from Tasmania to the Antarctic continent. Due to the layout of the major mountain systems on earth, the amount of water injected into the Pacific rivers only accounts for 1/7 of the total amount of water injected into the ocean by the rivers of the world. in the Pacific water system, the most important are the rivers of China and Southeast Asia. The Pacific Ocean Basin can be drawn as three zones. 1. East: the American Cordillera (Cordillera) mountain system from the north of Alaska, southward to Tierra del Fuego, in addition to the northernmost and southernmost section of the fjord coast of the island group and deep into the mainland of the Gulf of California, the coast is straight, the continental shelf is narrow, the important trench in the north of the Acapulco Trench, the south of the Peru - Chile Trench. 2. West: the part of the Asia Complex structure, zigzag coast, the eastern edge of the continent has a prominent peninsula, offshore a series of island arcs, the formation of numerous marginal sea. From north to south, there are the Bering Sea, Sea of Okhotsk, Sea of Japan, Yellow Sea, East China Sea and South China Sea. The outer edge of the island group has a series of trenches, north of the Kamchatka Trench, Thousand Islands Trench, Japan Trench, south of the Tonga Trench, Kermadec (Kermadec) Trench and so on.3. The central Pacific Ocean is a wide area of the sea basin, is the most stable crustal tectonic region, the depth of seawater is generally in the 4,570 meters (15,000 ft.) or so. East of 150°W is the East Pacific basin, and south of the line from the Central American Isthmus through the Cocos Ridge to the Galapagos Islands are the Peru-Chile and Southeast Pacific basins. Further south across the Southeast Pacific Rise is the Pacific-Antarctic Basin. The area between this basin and 150°W is the Pacific-Antarctic Ridge. At 150°180°W, from east to west, there are the Pacific Central Basin, the Mariana Basin and the Philippine Basin; between New Zealand and East Australia, there is the Tasman Basin, and to the south, there is the Macquarie Ridge, which is the submerged boundary between the Pacific Ocean and the Indian Ocean. The Pacific Ocean islands are numerous, mainly distributed in the western and central waters, according to the nature of the continental islands and ocean islands are divided into two categories. The mainland islands are generally linked to the mainland in terms of geological structure, such as the Japanese Islands, Taiwan Island, the Philippine Islands, the Indonesian Islands and the world's second-largest island, New Guinea, etc. The oceanic islands are divided into volcanic islands and coral islands. Ocean islands are divided into volcanic islands and coral islands. The Pacific Ocean in the central west of the vast sea, from west to east there are three major islands: Melanesia, Micronesia and Polynesia. Among them, the Melanesian Islands are mostly continental islands, the Hawaiian Islands in Polynesia are famous volcanic islands, and almost all of the Micronesian Islands are coral islands. The Pacific Ocean, because of its vast area and uniform body of water, has a climate favorable to the formation of planetary wind systems, especially in the South Pacific. The situation is different in the North Pacific, with sharp differences between the east and west coasts, with the sharpest contrast between the harsh winters of the east coast of Russia and the mild winters of British Columbia in Canada. The trade wind belt lies between the subtropical high pressure center and the equatorial windless zone in the eastern Pacific between 30°40° north and south latitudes. At mid-latitudes, the westerly wind belt and the polar easterly wind belt converge to form the sub-polar low pressure belt. The difference in temperature and humidity between the two belts is huge, and the fronts of the polar easterly wind belt are very violent, especially in winter. In the western Pacific Ocean (5°25°N latitude), east of the Philippines, the South China Sea and the East China Sea, between summer and fall, under the conditions of high temperature and high humidity, ultra-low-pressure centers are generated, and violent tropical storms, i.e. typhoons, are formed. In summer, the Asian continent is under low pressure, and the North Pacific air currents move toward the continent. In winter, the situation is completely opposite, forming a vast monsoon climate zone. The sea water temperature in the North Pacific Ocean is higher than that in the South Pacific Ocean because the South Pacific Ocean waters are more extensive and are influenced by icebergs and cold water masses in the Antarctic region. Seawater in the trade wind belt has a higher salinity than in the equatorial belt because there are more clouds and precipitation near the equator, there is no wind, and evaporation is less than in the trade wind belt. The salinity near the equator is less than 34; the northernmost sea has the lowest salinity, less than 32. The ocean currents in the Pacific Ocean move from east to west under the influence of the trade winds, forming the South and North Equatorial Warm Currents. In the axis between the north and south equatorial warm currents, there is an opposing equatorial countercurrent that flows from the east coast of the Philippines to the west coast of Ecuador. The North Equatorial Warm Current turns northward near the Philippines and flows eastward toward Japan in the famous Kuroshio Current; the tributaries of the North Equatorial Warm Current enter the Sea of Japan through the Tsushima Strait and are called the Tsushima Warm Current. The Kuroshio current turns to flow eastward near 160°E and is called the North Pacific Warm Current. The North Pacific Warm Current moves eastward to the west coast of North America and turns to flow southward, called the California Cold Current. This forms the North Pacific Gyre. In addition, the Bering Sea current flows southward, called the Kamchatka cold current, also known as the pro-tidal current, to the east of Honshu Island, Japan, and meets the Kuroshio current near latitude 36 ° north. South Equatorial warm current to the Solomons, after the southward flow into the East Australian warm current, folded to the east involved in the westerly drift, to the west of South America, latitude 45 ° south near the division into two branches, one to the east through the Drake Passage into the Atlantic Ocean; the other folded to the north, that is, Peru, the cold current. This forms the South Pacific Gyre. The Pacific Ocean is rich in resources. The Sea of Japan and the Sea of Okhotsk in the western Pacific Ocean are important fishing grounds, producing herring, cod, tuna, crab and so on. The Columbia River on the west coast of North America is famous for producing salmon. There are a large number of manganese nodules on the seabed, and the seawater can extract sea salt, bromine, magnesium and so on. The continental shelf is one of the world's richest petroleum resources, such as the southern waters of California, the Yellow Sea, the East China Sea, and Indonesia, southeastern Australia and other sea areas. The western Pacific coast has long been an area of high culture. But Europeans did not begin to explore this ocean until the 16th century. They sought access to the Pacific islands through Australia, the so-called 'Land of the South', and in 1513 the Spanish occupier Vasco Nunez de Balboa saw the vastness of the Pacific Ocean from the summit of Darien on the Isthmus of Panama. In the 17th century, the Dutch navigator Abel Ta *** an discovered Tasmania, New Zealand and Fiji, and in the 18th century, the English navigator Cork, the French navigator Louis-Antoine de Bougainville and others sailed in the Pacific Ocean. In the 19th century, Charles Darwin, a British naturalist, sailed around the world on the Beagle in 18311836 and made great contributions to natural science through his expeditions in the Pacific. Kraternaya Bay The Pacific Ocean extends from the Antarctic region in the south to the North Pole in the north, to Asia and Australia in the west, and to South and North America in the east. It accounts for about one-third of the earth's area and is the largest ocean in the world. Its area, excluding the neighboring territorial seas, is about 165.25 million square kilometers. It is twice the size and more than twice the water capacity of the second largest ocean, the Atlantic Ocean. The area exceeds the total land area of the Earth, including Antarctica. The average depth (excluding dependent seas) is 4,280 meters. The western Pacific Ocean has many territorial seas, from north to south for the Bering Sea, the Sea of Okhotsk, the Sea of Japan, the Yellow Sea, the East China Sea and the South China Sea. The great East Asian rivers Heilongjiang, Yellow, Yangtze, Pearl and Mekong all flow into the Pacific through the Sea of Belongings. The ocean floor east of 150o W longitude is more gentle than that in the west. Ridges in the western Pacific that are more than 600 meters underwater form archipelagos in some places. From the Aleutian Ridge in the northwest Pacific, it extends southward to the Chishima Islands, Ogasawara Islands, Mariana, Yap, and Palau; from Palau it extends eastward to Bismarck, the Solomons, and Santa Cruz; and finally from the Samoan Archipelago it extends southward to Tonga, Kermadec, Chatham, and Macquarie. The water temperature in the North Pacific is higher than in the South Pacific due to a higher ratio of land to sea in the north than in the south and the influence of the Antarctic land ice cap. The salinity of seawater in the windless and variable wind zones near the equator is lower than in the trade wind zones. The greatest influence on vertical currents in the Pacific Ocean is the cold water generated around the Antarctic continent. Dense seawater around the poles sinks and then spreads northward to make up most of the bottom of the Pacific Ocean. The deep cold water flows northward in the western Pacific in relatively distinct currents from near Antarctica to Japan. Tributaries of this deep-sea main current carry cold water eastward and then to the poles in both hemispheres. The deep-sea circulation is influenced by the subsidence of surface waters in the neighboring current convergence zones. In the Pacific Tropical convergence zone were in the north and south latitudes between 35o and 40o, the farther from the equator, the greater the depth of seawater subsidence, the most important convergence zone in the latitude of 55 degrees south to 60 degrees between.

Q: How big is the charm of love? Seek help from the gods

Ask what is love in the world, straight to teach people to live and die?" It is a classic sentence, straight to teach people to live and die together, what is love? What power in the world can be greater than the magic of love ah, will be to life and death to relative treatment.

How deep is the difference between like and love?

Like is light love, love is deep like...

Please adopt