关于”介绍龙脊山“英语作文范文4篇，作文题目：Intduction to Longji mountain。以下是关于介绍龙脊山考研英语范文，每篇作文均为真题范文带翻译。

高分英语作文1：Intduction to Longji mountain

In order to treat chback, there was a man who suddenly tned into a chback. He went to see a doctor. The doctor first applied ointment to him, and then the doctor sandwiched the hump beeen o pieces of wood.

The doctor pressed the block of wood tightly, and the eyes of the chback were exposed. The stupid people in the world were also looking for wealth. People ted their hands in ry possible transaction.

They didn't realize that n if they committed the most secret cmes, they would get harm than pfit. Just as the doctor let the chback eyes open, they would go to hell one day.

中文翻译：

§为了治疗驼背，曾经有一个人突然变成驼背，他去看医生，医生先给他涂上软膏，医生把驼背夹在两块木块之间。医生把木块压得很紧，驼背眼睛都露出来了，世界上蠢在寻找财富，人们在每一个可能交易中尝试他们手，他们没有意识到，即使他们最隐秘地犯罪，他们也会得到更多伤害而不是利润，就像医生让驼背眼睛睁大了一样，他们总有一天会下地狱。

万能作文模板2：龙脊山简介

The theory of plate tectoni descbes the movement of the lithosphere, which is a relatively hard outer layer of the earth, including all the crust and part of the underlying mantle. The lithosphere is divided into dozens of plates of different sizes and shapes. Generally speaking, the plates move with each other.

The mid ocean dge is such a boundary beeen plates. New lithosphec mateals are injected fm below. When plates diverge fm the mid ocean dge, they slide on the layers at the bottom of the lithosphere that are easier to yield.

Becse the size of the earth is basically constant, only if the number is the same In other places, the site of this destruction is another kind of plate boundary subduction zone, where one plate subducted below the edge of another plate and re integrated into the mantle. Both plate boundaes are related to flt s, earthquakes and volcanic activities, but the types of geological activities observed on these o boundaes are completely different. The concept of seafloor spreading actually preceded the theory of plate tectoni.

In the early stage, it descbed the formation and destruction of the seafloor, but it did not specify the hard lithosphere plate. This hypothesis was quickly confirmed becse under the se of maa under the mid ocean dge, the peodic rrsal of the earth's maetic field was recorded in the oceanic crust, and when the maa cooled and solidified, the fermaetic minerals in the maa moved along The direction and polaty of the maetic field are preserved in the maetized volcanic cks. The rrsal of the maetic field pduces a sees of maetic stps parallel to the axis of the ft valley.

Therefore, the oceanic crust can be used as a maetic tape to record the history of geomaetic field, and its width can be determined independently, and the stpe represents the speed of seafloor spreading.

中文翻译：

板块构造理论描述了岩石圈运动，岩石圈是地球一个相对坚硬外层，包括所有地壳和部分下伏地幔。岩石圈被分成几十个大小和形状各异板块，一般来说，板块之间是相互运动，大洋中脊就是这样板块之间边界，新岩石圈物质从下面注入，当板块从大洋中脊发散时，它们在岩石圈底部较易屈服层上滑动，因为地球大小基上是恒定，只有当相同数量岩石圈物质在其他地方，这种地点是另一种板块边界俯冲带一个板块俯冲到另一个板块边缘之下并重新整合到地幔中这两种板块边界都与断层、和火山活动有关，但是，在这两个边界上观察到地质活动种类是完全不同。海底扩张概念实际上先于板块构造理论，在早期，它描述了海底形成和，但它并没有指明坚硬岩石圈板块这一假设很快得到了证实，因为在大洋中脊下岩浆上升，地球磁场周期反转被记录在大洋地壳中，当岩浆冷却凝固时，岩浆中铁磁矿物沿着岩浆方向被磁化，向地磁场方向磁化，磁场方向和极保存在被磁化火山岩中。

磁场反转产生了一系列平行于裂谷轴线磁条。因此，海洋地壳可以作为一种记录地磁场历史磁带，可以地确定其宽度条纹表示海底扩张速度。

满分英语范文3：介绍龙脊山

The theory of plate tectoni descbes the movement of the lithosphere. The lithosphere is a relatively hard outer layer of the earth, including all the crust and part of the underlying mantle lithosphere (NIS is divided into dozens of plates of different sizes and shapes. Generally speaking, the plates move each other.

The mid ocean dge is a boundary beeen plates, and new lithosphec mateals are injected fm below As the blocks diverge fm the mid ocean dge, they slide on the yielding layers at the bottom of the lithosphere. Becse the size of the earth is essentially constant, only when the same amount of lithosphec mateal is elsewhere, the site of such destruction is another kind of plate boundary: one plate subducted below the edge of the other plate and re integrated into the mantle. Both plate boundaes are related to flt s, earthquakes and volcanic activity, but the geolo observed at these o boundaes The types of activities are completely different.

The concept of seafloor spreading actually preceded the oginal version of the plate tectoni theory. In the early s, it descbed the formation and destruction of the ocean floor, but it did not specify gid lithosphec plates. This hypothesis was confirmed.

Soon after, as maa se under the mid ocean dge, the peodic rrsal of the earth's maetic field was recorded in the oceanic crust, and the fermaetic minerals in the maa were recorded When the maa cools and solidifies, the fermaetic minerals in the maa will be maetized along the direction of the maa. The direction and polaty of the maetic field are preserved in the maetized volcanic cks. The rrsal of the maetic field pduces a sees of maetic stps parallel to the axis of the ft valley.

Therefore, the oceanic crust can be used as a maetic tape to record the history of geomaetic field, and its width can be determined independently, and the stpe represents the speed of seafloor spreading.

中文翻译：

板块构造理论描述了岩石圈运动，岩石圈是地球一个相对坚硬外层，包括所有地壳和部分下伏地幔岩石圈（nis被分成几十个大小和形状各异板块，一般来说，板块之间是相互运动，大洋中脊是一个板块之间边界，新岩石圈物质从下面注入，当板块从大洋中脊发散时，它们在岩石圈底部较易屈服层上滑动。由于地球大小基上是恒定，只有当相同数量岩石圈物质在其他地方，这种地点是另一种板块边界：一个板块俯冲到另一个板块边缘之下并重新整合到地幔中这两种板块边界都与断层、和火山活动有关，但是，在这两个边界上观察到地质活动种类是完全不同。海底扩张概念实际上先于板块构造理论最初版，在年代早期，它描述了洋底形成和，但它没有具体说明刚岩石圈板块，这一假设得到了证实不久之后，随着岩浆在大洋中脊下上升，在大洋地壳中记录到地球磁场周期反转，岩浆中铁磁矿物被磁化，当岩浆冷却和凝固时，岩浆中铁磁矿物就会沿着岩浆方向磁化，磁场方向和极保存在被磁化火山岩中。

磁场反转产生了一系列平行于裂谷轴线磁条。因此，海洋地壳可以作为一种记录地磁场历史磁带，可以地确定其宽度条纹表示海底扩张速度。

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