But guess the profundity is not really profound, but something that has a certain significance. When the ancient bluebird felt that the deep was staring at him, it was also a very real strange feeling, as if this deep distance under the bottom of the sea was really alive, with its own life, and it was watching the ancient blue bird listen to this insignificant boat in the wind and waves. The ancient bluebird grabbed Lanling's arm, and said loudly to him through the sound of the wind and waves: 'This thing under the sea seems to be alive!' ’

After Lanling heard the words of the ancient blue bird, he also looked under the surface of the sea, as if he wanted to see through this large area of sea water and waves, and see what was under the sea water, but there was still nothing to gain, so he could only shake his head at the ancient blue bird. The ancient blue bird knew that Lanling didn't feel anything, but the feeling of the ancient blue bird being condensed still existed, so she couldn't help but wonder, could it be that this gaze was just aimed at herself? But now is not the time to speak, Gu Blue Bird Whale You hid such a thought in your heart, glanced at Lan Ling, and then stared at the wind and waves, and continued to move in the direction of Abyss Island.

The old crew pilot, a small boat, spent a lot of effort through this turbulent area, and finally near the abyss island, the waves near the abyss island have become small, but they are still much bigger than the waves around the ordinary island, the old crew will stop next to the abyss island, and say to the ancient blue birds: "You go up, I want to stay here, there is no ferry here, there is no pier, there is no one to take care of here, you will soon be taken away by the waves, I know that you are not ordinary people, If you want to go up, there must be something very important, and I will not keep you anymore, I will show you the boat here, and when you come out, I will take you away. ”

Gu Qingniao and Lan Ling just didn't want outsiders to know about their search for that place, so they didn't refuse the kindness of the old crew, but after thanking the old crew, they walked towards the island. The address of the island is very special, the ground is full of stones, and the foundation of the stone forms the basic outline of the entire island, and the ancient bluebird reached out and picked up a piece of stone from the ground, and said, "This is granite?" ”

Lan Ling nodded and said, "Yes, this is granite. ”

Granite belongs to the intrusive rock in acidic (SiO2>66%) magmatic rocks, which is the most common type of rock of this kind, mostly light flesh red, light gray, grayish white, etc. Medium-coarse-grained, fine-grained, block-like structure. There are also some patchy structures, spherical structures, and gneiss-like structures. The main minerals are quartz, potassium feldspar and acid plagioclase, while the minor minerals are biotite, hornblende and sometimes a small amount of pyroxene. There are many types of secondary minerals, such as magnetite, zelder, zircon, apatite, tourmaline, fluorite, etc. The quartz content is the largest among all kinds of magmatic rocks, and its content can range from 20-50%, and a few can reach 50-60%. The content of potassium feldspar is generally more than plagioclase, and the relationship between the content ratio of the two is often that potassium feldspar accounts for two-thirds of the total feldspar, plagioclase accounts for one-third, and potassium feldspar is mostly light flesh red in granite, and there are also grayish white and gray. Off-white potassium feldspar and plagioclase are often indistinguishable on hand specimens. At this time, we need to carefully observe the double crystal characteristics of these two feldspars, because plagioclase feldspar has poly double crystals, and when we turn the hand specimen, we can see that there are regular light and dark clusters on the plagioclase crystals, while potassium feldspar is a cassette double crystal, which is characterized by two halves of crystals with different degrees of brightness. Granite can also be further named according to the dark mineral species, such as the dark mineral is mainly biotite, which can be called biotite granite, which is a common type of granite. If it is biotite and muscovite, its content is nearly equal, it can be called mica granite, if the dark mineral is dominated by hornblende, it is called hornblende granite, if the dark mineral is dominated by pyroxene, it is called pyroxene granite, and if it contains almost no dark minerals, it can be called white granite.

As the iconic rock of the continent, granite forms the foundation of the upper crust of the continent, and the formation process of granite is usually closely related to the tectonics, metamorphism and mineralization of the continent. Since the 18th century, when geological science was still in its infancy, the question of the genesis of granite has been the subject of much debate. For a debate on the origin of granite, see Gilluly (1948), Pitche

(1993) and You

G (2003) et al.'s treatises are not listed here. It should be mentioned that since the advent of plate tectonics theory in the 60s of the 20th century, many explanations for the origin of granite have been re-understood in the theoretical framework of plates. In many cases, there seems to be a convergence of understandings, but the actual debate continues. Bowe

(1914, 1922, 1948) is that the crystal sequence of minerals is combined with the sequence of magmatic rocks from mafic to acidic rocks. Experimental results show that the crystallization of basalt magma ultimately produces only a small amount of residual granitic melt, which clearly contradicts the fact that there are many granites in the field (Holmes, 1926, Read, 1957). The Mineral Reaction Series can actually be applied to magmatic systems of different compositions. In other words, the initial crystals from the magmatic system are not necessarily mafic rocks, and the final crystals are not necessarily felsic (acidic) rocks, because the properties of the rocks crystallized from the melt depend on the composition of the melt rather than the order in which the minerals crystallize (Ke

edy，1933)。 Walto

(1960) had to Bowe

"There is nothing wrong with Bowen's theory of chemistry or its application to the separation of basalt magma, which remains a fundamental principle of petrology. However, it would be a bit speculative to think that most of the evolution of igneous rocks is the result of the cooling, crystallization and separation of basalt magma into the earth's crust. The same chemical theory can be applied to other models" in the 40s of the 20th century (Gilluly, 1948) represented by H.H. Read and N.L. Bowe

The controversy between the "magma theorists" ended with the subsequent recognition of the magmatic origin of granite by more and more scholars. However, where does the magma that makes up the granite body come from? With Bowe

The words indicate: Whe

ce the g

a

ites? (Where does granite come from?) The overwhelming understanding of this question is that granite is formed by the melting and solidification of various parts of the earth's crust. This view is a combination of two different earlier theories about the origin of granite: the magmatic theory (the belief that granite comes from the crystallization of magma) and the metamorphosis theory (the view that granite is a silicon-aluminum-rich sedimentary rock modified by granitization under dry or water-bearing conditions). It is proposed that granite is the result of supermetamorphism (deep melting) of crustal rocks, which is of great significance for the study of the origin and chemical differentiation of the earth's crust, because they are related to the thermal state of the crust and the composition of the original rock in a specific period, including how much granite magma can be produced, the temperature and the amount and source of water when granite is formed, the tectonic background and the process of plate action, etc.

In order to properly understand the so-called "granite problem", it is necessary to first understand how qualitologists arrive at the conclusions that form the current doctrine. It is therefore necessary to systematically elaborate on the knowledge of ideas that have been around a century or more. From these narratives, it can be seen that many of the "new concepts" that have developed in the last two or three decades are the same topics that have been discussed and debated for the past 100 or 150 years. In the thirties of the twentieth century, geologists debated fiercely about which granites were magmatic and which were metamorphic or metasomatized. The controversy began as early as the time of the Hydrophobia, and until the middle of the nineteenth century, it was entangled in the idea that granite was formed by deposits in an aqueous solution. Although since Hutton (Hutto

), the process of metamorphism (a term proposed by Lyell) has been recognized, although its properties are not well understood. Even before the use of microscopes, much was written about the metamorphic formation of granite. Hutton himself was a strong advocate of the idea of magmatic genesis. According to Hutton, the characteristics of granite unconformity intrusive layered rocks, coarse-grained crystalline structures, and granite of oblique rock formations are all considered to be granite composed of "subte."

a

ea

lava)" evidence of the formation of crystallization, which the underground lava later called "magma". As for the behavior of magma, there are many situations that cannot be explained well if the presence of water is not assumed, and this has long been emphasized. This is especially important in the case of granite, so it is necessary to describe in advance a problem that was revived more than a decade ago. Sparantsny (Splla

za

i, 1794) may have been the first to recognize the genetic significance of the need for water to appear in molten rocks. Subsequently, Scholaup (Sco

p, 1825) had discussed the significance of water in lava, and Schee

e

et al., 1862) more explicitly linked the presence of water to granite magma. In addition, Bonson (Bu

se

Anderson et al., 1861) also discussed the geology of granite, especially the question of its genesis. At that time, it was known that the crystallization temperature of quartz in the molten state was higher than that of orthoclase, and much higher than that of mica. The "anti-fire theorists" do not admit that granite was formed by magma, and insist that if granite is indeed formed by magma, then the crystallization order of these minerals in granite should be quartz, orthoclase, and mica. As we all know, the actual crystallization order is exactly the opposite. It is thus proved that granite could not have been ignited. According to Bonson, the melting point of one mass is not the same as the temperature at which the matter crystallizes from its solution in another case. On the other hand, in further discussion, he made comparative work on the behavior of some chemical components in aqueous solutions. The concept of granitization (migration of acidic substances) dates back to the time of Lyer in 1836. At that time, the controversy over the cause of granite can be explained in the context of the Oslo area. Leopold von Bucher (Leopold

． Buch) surveyed the area in the early nineteenth century, while Charles Lyer in 1837 investigated the area in Kelho (B. Kelho). M, Keilhau) also conducted a survey of the area. Holtedah I (1963) has fully commented on these investigations. According to this account, von Bucher (a student of Werner) believed that most of the granite in this area was overlain by fossil-bearing structures in the same form as basalt and other "dark" rocks in general, while the D. drumming granite (D. D

amme

g

a

ite) is older than limestone and lies beneath limestone. However, Lyer was very skeptical of these explanations, arguing that there were places where granite could be obliquely overlain on sedimentary rocks, but this was a secondary feature, and it was generally the granite that extended out of the veins into the adjacent strata and turned the limestone into marble and the shale into mica schist. In essence, he adopted Hutton's concept of deep activity; Molten material violently invades older structures and causes thrust on the overlying rock mass. However, Keljo did not accept these notions, and he did not understand how such a large space could be open for the invading human body immersed in a place that was once occupied by eruptive rocks. As early as 1838, Kelhoe was probably the first to pay attention to the "spatial problem" of igneous rock invasion. Kelhoe proposed his "Turning Role" (t

a

**utatio

s) doctrine to replace the above ideas. The view of this argument is that the early rock masses were transformed into granite and syenite by a slow and steady process. Kelhoe calls this process "granite-making" (g

a

itificatio

)。 He also claimed to have found an example of a change from sedimentary rock to granite; For this change, he did not pay attention to the connection to the deep phenomenon, nor did he consider the temperature increase involved. However, Kje Roul (Kje

ULF, 1855, 1879) argued that the granite of Oslo was fire-born. He acknowledges the spatial problems raised by Keljo, but argues that the scorching intrusion has swallowed up the previous sedimentary rocks. Thus, the concept of "assimilation" was introduced in igneous petrology. Decades later, Michel-Levv (1894), who may not have known about the writings of Rolf at the tomb of Kai, invoked the concepts of metasomatism and assimilation in France when describing the genesis of granite. At the end of the nineteenth century, the concept that granite was formed by metamorphism and metasomatism prevailed in France. Educated in France and England, such as Kekirolf in Norway, the emphasis is on magmatic-ig

eous) said the point of view. In Finland, Seidholm (1893) turned out to oppose the Canadian Lawson (A. Lawso

Lawson has believed that the oldest granites that have penetrated into the original crust and the oldest sedimentary rocks were formed by the remelting of the oldest sediments at the bottom. Seidholm (1892) identified the ring-porphyry granite as a true magmatic rock that could be filled into a graben-like depression during periods of intense vertical movement (g

abe

-like dep

essio

s), and it was during this period that the ringpoise granite was intruded by large rock masses. Later, Seidholm developed his own concepts of regeneration and deep melt for other granites, which were in part consistent with Lawson's concepts in Canada. Tiger Stede (T/ge

Stedt, 1893) published a slightly different concept when describing some of the mixed rocks in southern Finland (which later became known as mixed rocks). He believed that the rocks were formed by granitic material penetrating into a metamorphosed sediment piece of gneiss. This granitic material contains a considerable amount of water, the presence of which accelerates the progress of the action and allows the granitic material to form fine veins that penetrate into the gneiss. Therefore, he reiterated the presence of water to explain the formation of fine-grained rock veins with narrow resistance and long distances; It would be quite difficult to explain their formation in other ways. In general, granite generally forms huge rock foundations. In fact, these foundations are rarely granite, but mostly composed of mountain granodiorite, steep rock, and quartz diorite. However, some granites are thought to form caps, basins or domes. Determining the occurrence of granite is an important issue, and the terminology used to describe the occurrence has a causal connotation to those who adopt it. According to Gilbert (Gil-be

T, 1877), the rock cap is the result of the upward movement of magma, and the meaning of the rock basin is the passive easement of magma into the space formed by the collapse of the chassis. The term rock foundation was recommended by Suess (1895); It is quite difficult to deduce the immersion desert type of a rock foundation. Hughes himself once compared the process of magma rising through the earth's crust with "red-hot tongs of fire to force its way through the plank." Still, this vivid metaphor is by no means an explanation (Levinson-Lexing). Kekirolf (1855) and Michiel-Levi suggested that the rock mass was formed by the gradual assimilation of magma into the surrounding rock, and the rate at which magma rose depended on the speed at which magma digested the surrounding rock and roof. Later, in 1923, Cloos argued that many of the rock masses that had been assumed to be rocks were in fact large intrusive beds, and that the intractable spatial problem was no longer a problem for the intrusion of the rock beds. In the dome structure, there is often a granitic core surrounded by gneiss. Finnish geologist Gadoli

, 1858) was the first to describe Pusu

saa

i) Man in the rock dome structure in the northern part of Lake Ladoga. According to his opinion, the rock dome structure is the intrusion of granite rock mass under the mountain, the inclination angle of the upper contact surface is gentle, and the downward angle gradually increases, and the intrusion structure remains gentle and the outward inclination from the core decreases. In 1951 Escola explained the dome as follows: "As summarized in my 1949 paper, it has been shown that granitization, with the addition of a large amount of potassium and an increase in volume, has specially modified the marginal part of the rock mass, causing the ancient intrusion to uplift and penetrate the dome".

The granite is extremely strong, basically the basic structure formed by the continent, and it is very stable, and the first dam in China is a building built on the whole granite, so it can ensure that it can maintain stability for hundreds of years. The site of the Three Gorges Dam was selected through a large number of geological explorations and 24 years of scientific demonstration, where not only the river valley is open, but the most important thing is that the bedrock in this area is hard and intact granite, and it has superior topography, geology and construction conditions for the construction of concrete gravity dams. If the foundation is not solid, not to mention the strong water pressure of the Three Gorges Reservoir, even the Three Gorges Dam with a volume of more than 16 million cubic meters and a weight of about 40 million tons will not be able to withstand it (concrete is calculated at 2.5 tons per cubic meter). Although the bedrock where the Three Gorges Dam is located belongs to hard granite, it cannot be said that the entire Three Gorges Reservoir area is granite geology, and in fact, the reason why the surging waves of the Yangtze River can cut through Wushan and form the world-famous Three Gorges of the Yangtze River (Qutang Gorge, Wuxia and Xiling Gorge) is precisely because Wushan, which runs through the border area between Hubei and Chongqing and other provinces and cities, belongs to limestone geology, and the water flow of the Yangtze River can erode it and cut deep into the river valley. And because Wushan belongs to a typical karst landform mountainous area, due to the extremely complex geological environment, the dark river karst caves are all over, when the Yiwan Railway was repaired, there was no less trouble, and the most difficult time was only 4 meters a month, which is why the average cost per kilometer of the Yiwan Railway is more than twice that of the Qinghai-Tibet Railway. Although there are many karst caves in Wushan and its vicinity, with the normal impoundment of the Three Gorges Reservoir, the water level of the river channel is raised, many karst caves in the reservoir area are submerged, and the dark river is also submerged or irrigated, and the drop is small, so the effect of groundwater on the dissolution of rocks is weakened, and with the decrease of water flow speed, some sediment is also continuously deposited in these places. In short, the construction of the Three Gorges Dam is, as a well-known Swiss hydropower expert put it, "a gift from God to the Chinese."

This reminds the ancient bluebird of Verne's novel "The Mysterious Island", and the small island in the mysterious island is a granite landform. The story tells the story of several northerners who were trapped in the Confederate army during the American Civil War, and were blown down by a storm on a desert island in the Pacific Ocean. They were not rescued until the Duncan, commanded by Captain Grant's son Robert, passed by; After returning to the United States, these "islanders" resumed the work they had established on the island. The novel combines reality and fantasy, with twists and turns, full of descriptions of the bizarre and colorful natural world, and a thrilling story that blends all kinds of knowledge. The work is imbued with optimism, believing that the infinite creativity of mankind and the great power of science will enable mankind to build an ideal society. The time span of "The Mysterious Island" is from 1875 to 1878, with the American Civil War as the social background, showing the individual as a duckweed in society, deeply affected by the changes in society, politics and economy. The setting of this background is inseparable from Verne's life experience: his life has experienced major historical events such as the 1848 Revolution, the Franco-Prussian War, the Paris Commune, and witnessed the peaceful development of capitalism, until he entered the stage of imperialism. And as the mark of that era. At the same time, his thoughts also reflect the ideological tendencies and value orientations of that era. In this work, the author makes the storyline he writes, the struggle between man and nature on a desert island, the technological innovation, and the creative labor from scratch, all deeply attract the reader. In the work, Smith and the other five people fled to a desert island, but they did not despair, but united, and everyone elected Engineer Smith as the leader and began the life of a primitive society. Eventually, they returned to their homeland aboard the Duncan and bought a piece of land with the property left behind by Captain Nemo, and they were still united. Captain Nemo sails alone to Tabo Island, thousands of miles away, when he is terminally ill, and in the middle of the Pacific Ocean, he leaves a note to save five people on the island, which is a sign of selfless dedication. The fact that five people were able to leave the desert island before the volcanic eruption was a sign of Captain Grant's sons and daughters keeping the promise they made thirteen years ago, which is a manifestation of their credibility as human beings. The book distinguishes between good and evil, punishes evil and promotes good, and the work is imbued with the spirit of optimism, believing that the infinite creativity of mankind and the great power of science will enable mankind to build an ideal society. The five main characters in the book are engineers, sailors, cooks, etc., and the author uses the portrayal of these characters to show readers the spirit of the American Northerners. Although the characters in the book have different occupations and personalities, they all share a love of life and a spirit of adventure. It is this spirit that gives them the courage to live on a desert island and the confidence to overcome all difficulties; It is this spirit that inspires these people to use their hands to change the land and turn Lincoln Island into a paradise. In the book, Elton is first exiled, exiled to an isolated island, and finally reborn with the help of the Smith Five. This story takes place in the colonial era, and the "inhumane" and "humane" reasons behind the change in the trajectory of his life make the story of a prodigal son turn back with particularity and profundity. After all kinds of twists and turns on the island, Elton finally lived with the settlers, and was finally able to return to society due to the difficulty of Elton's integration, which proved the strong appeal of humanitarianism on Lincoln Island. The work embodies the author's view of colonial society. This can be seen from the conversation between Cyrus Smith and Nemo in "The Mysterious Island". Nemo, a hero of colonial rule who had rammed and sunk a British destroyer at sea, said: "I have both the right and the right to do so." I always try to do good as I can, but I also do evil when I need to. Justice is not the same as forgiveness! Cyrus Smith's answer was quite representative of Verne's voice: "Captain, your mistake is that you think you can reproduce the past, and try to resist the inevitable progress. This mistake has been appreciated by some and condemned by others, and only God can adjudicate on it, and it deserves to be forgiven. One can attack those who do wrong things with good intentions, but one cannot fail to respect them. Your mistakes do not prevent others from respecting you, and your name does not have to worry about the judgment of history. History loves crazy heroic deeds, although it also condemns the consequences of such deeds. Here, colonization is seen by Verne as an "inevitable progress" of history, and the ambivalence of both "respect" and "condemnation" of Nemo's rebellion is reflected in his colonial outlook. So Verne conceived of Lincoln Island, the perfect example of a colony, where even the Christian ideal ——— salvation of sinners could be realized. Lincoln Island sank, and the settlers "lay on the reef, dying, completely oblivious to what was happening around them." Only Elton still used his last strength to raise his head and look desperately at the uninhabited sea! He eventually spotted and signaled to the Duncan for help. Jean-Jules Verne, grandson of Verne, commented: "Of all those who lay on the reef with only one breath left, only Elton, who had suffered social ostracism, raised his head, and he did not lose all hope, and finally found the Duncan; And all Cyrus Smith could do was shout: 'Ah! God Almighty! You have shown mercy and saved us! The symbolism of this scene is striking: it is the repentant sinner who receives the message, and it is the scholar who succumbs to the power of the universe. "The writing of the novel is smooth and fresh, full of delicate and vivid descriptions of the colorful and magical scenery of the natural world, and reveals a heartfelt love for the magnificent and magical nature. In addition, while fully celebrating the great creativity of human beings in the struggle against nature, it also expresses admiration and awe for nature. The success of "The Mysterious Island" lies not only in the ups and downs of the plot, the realistic portrayal of the characters, the perfect combination of fantasy and science, but more importantly, the humanist spirit and patriotism that run through the whole book. In this work, the author makes the storyline he writes, the struggle between man and nature on a desert island, the technological innovation, and the creative labor from scratch, all deeply attract the reader. The work is imbued with optimism, believing that the infinite creativity of mankind and the great power of science will enable mankind to build an ideal society. There are five main characters in "The Mysterious Island", and the author does not have many positive descriptions of them, but as the story unfolds and the plot deepens, the different personality traits of these characters are vividly presented to the reader: the intelligent, erudite and resolute engineer Cyrus Smith, the knowledgeable and well-mannered New York Herald war correspondent Gidding Spellley, the kind and adventurous sailor Pancrof, the talented and studious young Herbert, and the loyal, gentle, and ingenious black Naboo. In addition, there is Elton, a former criminal who has reformed and is hardworking and humble. In the novel, they unite and learn from each other's strengths and weaknesses to form a perfect collective. Among them, the engineer Cyrus occupies a pivotal position, he is the leader and soul of the entire colonization team, and is also the embodiment and symbol of the idea of "man conquers heaven" in Europe in the nineteenth century with the development of science and technology. "The Mysterious Island" inherits the usual characteristics of Verne's science fiction novels: unreal but not too detached from reality. His fantasies are all based on scientific knowledge, so they don't make people feel unattainable. He skillfully integrates a wealth of scientific knowledge into his works, so that readers are naturally influenced by popular science knowledge in the process of appreciating the story, which contains metallurgy, blastology, engineering, hydraulics, flora and fauna, astronomy, physics and other aspects of scientific knowledge, making this work both fascinating and extremely educational.

Jules Verne was a 19th-century French novelist, playwright, and poet. Born into a middle-class family in the French port city of Nantes, Verne studied law in Paris at his father's behest, and later began writing plays and magazine articles. During his collaboration with the publisher Herzel and his sons, from 1862 until Verne's death, Verne's literary career was a great success, and many of his works were translated into many languages. Verne wrote a large number of excellent literary works during his lifetime, with the general title of "Strange Travels in the Known and Unknown Worlds", which is represented as a trilogy "Captain Grant's Children", "20,000 Leagues Under the Sea", "The Mysterious Island", "Five Weeks in a Balloon", "Journey to the Center of the Earth" and so on. His work had an important influence on the genre of science fiction, so that, along with Herbert George Wells, he is known as the "father of science fiction". [1] According to UNESCO, Verne is the second most translated artist in the world, after Agatha Christie, and ahead of Shakespeare. According to UNESCO's recent statistics, Verne has been translated into 4,751 works worldwide[2] and he was the most translated French writer in the world in 2011. In France, 2005 is designated as the year of Verne to commemorate the centenary of his death.

Science fiction fiction did not begin with Verne, but Verne greatly surpassed his predecessors in the scale of fantasy, especially in the linguistic nature of science. Verne's talent lies in the fact that, within the limits of science and technology, he made all sorts of ideas that were incomparably wonderful at the time according to the laws and inevitable trends of scientific development. Because these ideas were in line with the trend of science, almost all of them became a reality by the 20th century. Verne's attitude towards science was serious, and he based his imagination on science as much as possible, for example, in order to write the story of the flight from the earth to the moon, he first carefully studied the scientific and technological problems such as aerodynamics, flight speed, weightlessness in space, and the splashing of objects. It is on this basis that his science fantasy is a prophecy of science. At the same time, Verne's works are not dry scientific illustrations, but are essentially of the nature of Romantic literature. He has always wove complex, tortuous and intriguing stories within the framework of scientific imagination, with thrilling plots full of strange coincidences, and then lined with extraordinary natural wonders, resulting in a strong romanticism, and Verne's smooth writing and brisk narration.

Verne's work is full of obvious social tendencies. At the same time full of knowledge, but he himself is a cosmic mystic and has a mystical cult of the world. In his novels, sometimes the questions are not deep enough, and the themes are often repetitive.

Verne's works not only have a unique artistic charm, but also have a profound impact on real life, and the images of scientific warriors and pioneers in his novels have influenced generations of followers. Many scientists admit that they were inspired by Verne to embark on the path of scientific exploration. The first words of Simon Lake, the inventor of the submarine, in his autobiography were "Jules Verne was the general director of my life's work"; Rear Admiral Bird, after flying over the North Pole, said Verne was his leader; Picard, the balloon and deep-sea explorer, and Makeni, the inventor of the radio, agreed that Verne was the one who inspired their inventions. Verne not only denied that he was the inventor of undersea navigation, but also claimed that he had never had a particular interest in science – but "only a special interest in using it to create dramatic stories that took place in foreign lands." "In fact, his reputation as the father of science fiction has led to a serious blurring of his literary value."

After the ancient blue bird saw this, they immediately began to die, this island is an island caused by geological activity or continental subsidence, not a volcanic island, so such an island is stable and solid, and the entire continental shelf is connected, although it is in the deep sea, but it does not recover the impact of huge waves and earthquakes, and basically there will be no unexpected disappearance. That's why it's been here for so long, and it's chosen as the place to hide your place.

When the ancient bluebird raised his head, he saw that all the scenery on the whole island was the same, full of jagged rocks, occasionally flat, also rocky ground, there was very little sand on it, only some of the mud blown by the sea breeze remained in the crevices of the rocks, as if it were a rocky beach after a flood. Gu Qingniao walked among these rocks, basically there is no place to stay, but now the strength of Gu Bluebird's body is not comparable to ordinary people, so it is quite easy, the two of them carry backpacks, and then move towards the center of the island, because this island only has a large momentum, and there is no distinctive landform at all, Gu Bluebird and Lanling guessed that the key place should be in the middle of this island, but if it is no longer in the center, it should have no impact, After all, the island is so big, it doesn't take much time to find it again, and it will be very convenient to start looking for it from the middle.

Gu Qingniao and Lanling came to the very center of the island, and sure enough, they saw a depression that was slightly different from other places, and this depression was particularly abrupt, as if it had suddenly appeared in this rock. The ancient bluebird they believe more and more, this is where the place is, after all, in the humming song islands are made of oil granite, the sudden appearance of the depression, if not the magic of nature, then it must be artificially dug If someone really digs a big pit in this place where the bird does not, then obviously their intentions are very far-reaching.

Gu Qingniao and Lanling glanced at each other, walked towards the depression in the center of the island, and sure enough, they saw that there were many stones placed in this depression on the island, these stones have a long history, but they are not from the same origin as the stones on the ground, maybe ordinary people look no different, but Gu Qingnao and Lanling can feel it with you, and the more ancient atmosphere on these stones makes them secretly surprised in their hearts. The presence of such an ancient aura on these stones is enough to illustrate the extraordinaryness of the ionic qualified place. Gu Qingniao stretched out his hand and stroked these stones, and suddenly felt the energy running inside, and he was surprised: "This is the eye of a formation?" ”

Lan Ling nodded: "It seems to be so." ”