有关地球的英语作文_初二高分英语作文3篇
关于”有关地球“英语作文范文3篇，作文题目：About the earth。以下是关于有关地球初二英语范文，每篇作文均为高分范文带翻译。
高分英语作文1：About the earth
When the earth is formed, it is basically a mixte of vaous cks. If the accumulation pcess continues, the decay of radioactive elements and kinetic ener of solid particles within a short life span will not exceed the average temperate of the earth. It is preliminaly estimated that it will not exceed the average temperate of the earth.
Therefore, the earth is solid after its formation. Due to the release of long-lived radioactive mateal decay and gravitational potential ener, the internal temperate ses slowly, indicating that the pmitive earth contains Some in oxides will be reduced into liquid in, and some in oxides will also be reduced to the liquid in, which will flow into the heart and form the core due to its high density (this pcess started and has not finished yet. There are different opinions becse the concentration of heavy mateals on the release potential can make the earth's temperate about centigrade, which pmotes the chemical differentiation pcess, the crust mantle cks thugh weatheng and air and water The latter is influenced by temperate, presse and metamorphi, as well as the formation of metamorphic cks.
These cks may first undergo peodic melting and consolidation to form the core of the continent. Later, the oginal earth gwing on the continent may not be able to preserve the atmosphere and ocean. They are secondary oceans and within the earth When green plants appear, they use the solar radiation to photosynthesis of water vapor (H2O) and CO2, resulting in the pduction of oric matter and free oxygen.
When free oxygen is slowly accumulated, it forms a large amount The main nitgen and oxygen in the gas.
中文翻译：
℃地球形成时基上是各种石头混合物，如果聚积过程继续进行，短寿命内放元素衰变和固体粒子动能都不超过地球平均温度，初步估计不超过度，所以形成后都是固态，由于释放长寿命放物质衰变和重力势能，内部缓慢升温，说明原始地球中含有铁被为液态，一些氧化铁也会被还原℃液态铁，因为其密度高而流入心脏，形成地核（这个过程始于，现在还没有结束，有不同意见是由于重物质对释放电位浓度能使地球温度约为摄氏度这促进了化学分异过程，被壳幔岩石通过风化作用和空气和水侵蚀，沉积岩和沉积岩分开，后者由地下排出气体和溶液，受温度、压力和变质作用影响，以及变质岩形成，这些岩先可能经历周期熔融和固结，形成大陆核心，后来成为大陆生长原始地球可能无法保存大气和海洋，它们是次生海洋是地球内部适度增加结果，但大气形成过程比较复杂H2OCO原始大气可能会还原，当绿植物出现时，它们利用太阳辐使水蒸气（H2O）和CO2进行光合作用，导致产生有机物和游离氧时，氧气产生量大于消耗量，自由氧是缓慢积累，在漫长地质时期，它形成了大气中主要氮和氧。
万能作文模板2：关于地球
Mystery of the ogin of the moon: for the ogin of the moon, scientists have pposed three theoes: capte theory, homolo and earth splitting, both of which are flawed, saying, but Apollo will pve that this seems to be the most unlikely theory that some scientists beli is the best theory that the moon and the earth, fm a set of coic dust generators, another theory is that the moon is the earth The "child" of the ball may be the Apollo lunar exploration "dug out" fm the Pacific Ocean. The results show that the composition of the earth and the moon are very different. Some scientists put forward another hypothesis, namely "capte".
They think that the moon intrudes into the gravitational field unintentionally and is locked in the crent orbit. It is extremely difficult to explain the mechani of this pcess theoretically. Therefore, the above three hypotheses are extremely difficult As Dr.
Robin Harlem said, "to explain the absence of the moon, there is an easier" mystery of the moon's age "than to explain the existence of the moon: spsingly, ck samples retned fm the back of the moon. After ysis, it was found that the age was about 10% of the earth's age. Armstng picked up the first piece after landing in the" peaceful ocean " The age of the cks is 100 million years ago.
Other cks are billion years old. They have a history of one billion years and a history of sral billion years. Almost all of the oldest cks on the earth are lunar cks whose age was determined to be one billion years at the world lunar Symposium one billion years ago.
What's , these ancient cks were collected fm scientists according to the data Scientists beli that it is the youngest area on the moon. Some scientists have pposed that the lunar soil formed in interstellar on earth not long ago was older than cks, and a bigger mystery: the ancient cks of the moon have left scientists at a loss, howr, compared with these cks.
中文翻译：
月球起源之谜：对于月球起源，科学家们提出了三种理论：捕获说，同源和地球它们都有缺陷，说，但阿波罗将帮助证明，这似乎是最不可能理论是一些科学家认为最好理论，月球与地球在十亿年前，从一组宇宙尘埃发生器另一个理论是，月球是地球“孩子”，也许是太平洋“挖”出来阿波罗探月结果显示，地球和月球成分差别很大，有科学家提出了另一个假设，即“俘获”他们认为月球是无意中闯入引力场，而被锁定在目前轨道上，从理论上解释这个过程机理，是极其困难，因此，上述三个理论都很难成立，正如罗宾·哈勒姆博士所说：“要解释月球不存在，月球存在比解释月球存在更容易“月球年龄之谜”：令人惊奇是，岩石样从月球背面返回，经分析发现，年龄约为地球年龄百分之十，阿姆斯特朗在“宁静海洋”登陆后捡到第一块岩石年龄是亿年前另一些岩石年龄为亿年，有十亿年历史和几十亿年历史几乎还有地球和太阳系身，地球上最古老岩石是十亿年前在世界月球讨论会上被一个年龄确定为十亿年月球岩石更令人惊讶是，这些古老岩石是从科学家那里收集来，据科学家认为是月球上最年轻地区，有科学家提出月球在地球上不久前在星际空间形成月球土壤形成年代比岩石还要古老更大谜团：月球古老岩石已经让科学家束手无策，然而，与这些岩石相比。
满分英语范文3：有关地球
When the earth is formed, it is basically a mixte of vaous cks. If the accumulation pcess continues, the decay of radioactive elements and kinetic ener of solid particles within a short life span will not exceed the average temperate of the earth. It is preliminaly estimated that it will not exceed the average temperate of the earth.
Therefore, the earth is solid after its formation. Due to the release of long-lived radioactive mateal decay and gravitational potential ener, the internal temperate ses slowly, indicating that the pmitive earth contains Some in oxides will be reduced into liquid in, and some in oxides will also be reduced to the liquid in, which will flow into the heart and form the core due to its high density (this pcess started and has not finished yet. There are different opinions becse the concentration of heavy mateals on the release potential can make the earth's temperate about centigrade, which pmotes the chemical differentiation pcess, the crust mantle cks thugh weatheng and air and water The latter is influenced by temperate, presse and metamorphi, as well as the formation of metamorphic cks.
These cks may first undergo peodic melting and consolidation to form the core of the continent. Later, the oginal earth gwing on the continent may not be able to preserve the atmosphere and ocean. They are secondary oceans and within the earth When green plants appear, they use the solar radiation to make water vapor (H2O) and CO2 photosynthesis, resulting in the pduction of oric matter and free oxygen.
When free oxygen is slowly accumulated, it forms a large amount The main nitgen and oxygen in the gas.
中文翻译：
℃地球形成时基上是各种石头混合物，如果聚积过程继续进行，短寿命内放元素衰变和固体粒子动能都不超过地球平均温度，初步估计不超过度，所以形成后都是固态，由于释放长寿命放物质衰变和重力势能，内部缓慢升温，说明原始地球中含有铁被为液态，一些氧化铁也会被还原℃液态铁，因为其密度高而流入心脏，形成地核（这个过程始于，现在还没有结束，有不同意见是由于重物质对释放电位浓度能使地球温度约为摄氏度这促进了化学分异过程，被壳幔岩石通过风化作用和空气和水侵蚀，沉积岩和沉积岩分开，后者由地下排出气体和溶液，受温度、压力和变质作用影响，以及变质岩形成，这些岩先可能经历周期熔融和固结，形成大陆核心，后来成为大陆生长原始地球可能无法保存大气和海洋，它们是次生海洋是地球内部适度增加结果，但大气形成过程比较复杂h2oco原始大气可能会还原，当绿植物出现时，它们利用太阳辐使水蒸气（h2o）和co2进行光合作用，导致产生有机物和游离氧时，氧气产生量大于消耗量，自由氧是缓慢积累，在漫长地质时期，它形成了大气中主要氮和氧。