关于”有关介绍地球“的英语作文模板3篇，作文题目：About introducing the earth。以下是关于有关介绍地球的xx年级英语模板，每篇作文均为万能模板带翻译。
高分英语作文1：About introducing the earth
Early in the morning, we all set out to the seaside and took a lot of photos on the way. At noon we arrived at the hotel. After lunch there, we went to the beach.
We were so tired that we lay on the beach all afternoon, swimming on the way back to the hotel, and on the rainy night we went shopping for presents. We all stayed in the hotel and played billiards. I had a good time today.
中文翻译：
一大早，我们都出发去海边，路上拍了很多照片。中午我们到了酒店。在那里吃过午饭后，我们去了海滩。
我们累得整个下午都躺在沙滩上，在回酒店的路上游泳，下雨的那天晚上我们去买礼物。我们都住在旅馆里玩桌球。今天玩得很开心。
万能作文模板2：
When the earth is formed, it is basically a mixture of various rocks. If the accumulation process continues, the decay of radioactive elements and kinetic energy of solid particles within a short life span will not exceed the average temperature of the earth. It is preliminarily estimated that it will not exceed the average temperature of the earth.
Therefore, the earth is solid after its formation. Due to the release of long-lived radioactive material decay and gravitational potential energy, the internal temperature rises slowly, indicating that the primitive earth contains Some iron oxides will be reduced into liquid iron, and some iron oxides will also be reduced to the liquid iron, which will flow into the heart and form the core due to its high density (this process started and has not finished yet. There are different opinions because the concentration of heavy materials on the release potential can make the earth's temperature about centigrade, which promotes the chemical differentiation process, the crust mantle rocks through weathering and air and water The latter is influenced by temperature, pressure and metamorphism, as well as the formation of metamorphic rocks.
These rocks may first undergo periodic melting and consolidation to form the core of the continent. Later, the original earth growing 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 production of organic matter and free oxygen.
When free oxygen is slowly accumulated, it forms a large amount The main nitrogen and oxygen in the gas.
中文翻译：
℃地球形成时基本上是各种石头的混合物，如果聚积过程继续进行，短寿命内放射性元素衰变和固体粒子动能都不超过地球的平均温度，初步估计不超过度，所以形成后都是固态的，由于释放长寿命放射性物质衰变和重力势能，内部缓慢升温，说明原始地球中含有的铁被转化为液态，一些氧化铁也会被还原℃的液态铁，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，有不同意见的是由于重物质对释放电位的浓度能使地球的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的侵蚀，沉积岩和沉积岩分开，后者由地下排出的气体和溶液，受温度、压力和变质作用的影响，以及变质岩的形成，这些岩石首先可能经历周期性的熔融和固结，形成大陆的核心，后来成为大陆生长的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的结果，但大气的形成过程比较复杂h2oco原始大气可能会还原，当绿色植物出现时，它们利用太阳的辐射使水蒸气（h2o）和co2进行光合作用，导致产生有机物和游离氧时，氧气的产生量大于消耗量，自由氧是缓慢积累的，在漫长的地质时期，它形成了大气中主要的氮和氧。
满分英语范文3：有关介绍地球
When the earth is formed, it is basically a mixture of various rocks. If the accumulation process continues, the decay of radioactive elements and kinetic energy of solid particles within a short life span will not exceed the average temperature of the earth. It is preliminarily estimated that it will not exceed the average temperature of the earth.
Therefore, the earth is solid after its formation. Due to the release of long-lived radioactive material decay and gravitational potential energy, the internal temperature rises slowly, indicating that the primitive earth contains Some iron oxides will be reduced into liquid iron, and some iron oxides will also be reduced to the liquid iron, which will flow into the heart and form the core due to its high density (this process started and has not finished yet. There are different opinions because the concentration of heavy materials on the release potential can make the earth's temperature about centigrade, which promotes the chemical differentiation process, the crust mantle rocks through weathering and air and water The latter is influenced by temperature, pressure and metamorphism, as well as the formation of metamorphic rocks.
These rocks may first undergo periodic melting and consolidation to form the core of the continent. Later, the original earth growing 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 production of organic matter and free oxygen.
When free oxygen is slowly accumulated, it forms a large amount The main nitrogen and oxygen in the gas.
中文翻译：
℃地球形成时基本上是各种石头的混合物，如果聚积过程继续进行，短寿命内放射性元素衰变和固体粒子动能都不超过地球的平均温度，初步估计不超过度，所以形成后都是固态的，由于释放长寿命放射性物质衰变和重力势能，内部缓慢升温，说明原始地球中含有的铁被转化为液态，一些氧化铁也会被还原℃的液态铁，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，有不同意见的是由于重物质对释放电位的浓度能使地球的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的侵蚀，沉积岩和沉积岩分开，后者由地下排出的气体和溶液，受温度、压力和变质作用的影响，以及变质岩的形成，这些岩石首先可能经历周期性的熔融和固结，形成大陆的核心，后来成为大陆生长的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的结果，但大气的形成过程比较复杂H2OCO原始大气可能会还原，当绿色植物出现时，它们利用太阳的辐射使水蒸气（H2O）和CO2进行光合作用，导致产生有机物和游离氧时，氧气的产生量大于消耗量，自由氧是缓慢积累的，在漫长的地质时期，它形成了大气中主要的氮和氧。
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