What is Ma er Lake called, and where is Xinjiang Mahu Lake?

Lake Maar, the exact translation is Lake Maar. Maar (English maar, Latin mare), meaning swamp or lake, is the name of the people who live in the Rhine region of Germany. In the 19th century, German scientists discovered a very unique crater lake in the Eifel plateau in western Germany, because there was no second place found at that time, so it was named after the local customary name, and since then there has been Lake Mar in the world.

So far, there are two Mar lakes found in the world, one in Maar, Germany, and the other in Zhanjiang, China.

There are two main characteristics that distinguish Lake Marr from other volcanic lakes: first, the mode of eruption; The second is the relative height of the lake level to sea level. I will not go into detail here.

However, it should be pointed out that the recommended answer to this question (see above) explains Marlch as incomprehensible and misleading.

After the eruption of the Huguangyan volcano 150,000 years ago, the crater depression accumulated water into a lake. The eruption sediment is very well preserved, and the various flow structures of the eruption are very obvious, and they are damaged by fault structures after diagenesis, which can be seen everywhere, which provides a sufficient basis for the study of volcanic diagenesis and neotectonic movement. Huguangyan is a more typical "Maer Lake" found in China at present, which is relatively rare in the world, the sediment at the bottom of Maer Lake is 50 meters thick, it truly records the changes of paleoclimate and paleoenvironment in the modern era of the earth for more than 100,000 years, and is an excellent place for China to study the formation mechanism of Ma'er volcanic eruption and Ma'er Lake.

Xinjiang Mahu Lake is located in the Junggar Basin, which has great potential for oil and gas resource exploration and is an important successor area for the growth of production and reserves of Xinjiang Oilfield Company. In recent years, the pace of oil and gas exploration in the Junggar Basin has been accelerating, and more than 1 billion tons of large-scale reserves have been discovered in the Mahu area and Jimsar respectively.

The 1 billion ton oilfield in Mahu is the largest oil and gas exploration achievement in China in recent years, and has become the most realistic replacement area for increasing reserves and production in China.

Xinjiang Mahu SpecificsXinjiang Mahu Where is Xinjiang Mahu Specific?

Where is Xinjiang Mahu!

In Ruoqiang County, on the edge of the Gurbantong Desert in the southern Xinjiang Junggar Box Land.

Lake Mar is Latin for "mare", meaning sea.

1. Interpretation of Lake Marr:

In the early 19th century, German scientist Steininger first began to study the small and round crater lake on the Eiffel Plateau in western Germany, and defined Mar as a volcanic type.

Today, Lake Mar refers to a crater lake of unique origin, and the most typical Lake Mar in the Eiffel of Germany and Guangdong of China are the most typical of the world, such as the lake light rock in the Zhanjiang Park of the Leiqiong Global Geopark.

2. Characteristics of Mamaqier Lake:

Lake Marr is a crater lake, but it is different from other crater lakes in that it is characterized by its low, flat crater and no volcanic cone. This is due to the fact that, unlike ordinary volcanoes, the Mar volcano is the product of a steam-magma eruption. Underground magma heats the groundwater in the underground aquifer, which in turn forms steam, which erupts with the magma.

These eruptions, mixed with dirt and debris from the upper part, accumulate around the crater to form a ring of bulges called the ring of gushing tuff, which is called the Mar volcano.

The formation process of Lake Mar and scientific research:

1. The formation process of Lake Marr:

1.The upwelling of hot magma in the ground meets the groundwater in the aquifer, vaporizing the groundwater and creating a strong pressure;

2.When the pressure reaches enough to break through the surface, it will be destroyed**, forming a steam-magma eruption;

3.When the magma cools and the volcanism stops, a crater is blasted out of the flatland, and the eruption accumulates a ring-shaped bulge around the crater - a ring of gushing tuff, which is the Mar volcano;

4.The crater was blocked and water accumulated, and Lake Mar was formed.

2. Scientific research at Lake Marr:

1.Lake Mar is a closed lake with no rivers flowing in and out, and the hydrological and sedimentary systems are relatively simple, which can help interpret paleoclimate and paleoenvironmental changes.

2.When Lake Marr was formed, the site of steam** and eruption was generally located hundreds of meters underground, resulting in a large depth and thick sediment that could provide a stable sedimentary record for tens of thousands or even millions of years.

3.The "deep-water and anaerobic" environment of Lake Mar makes the sediment less disturbed by waves and benthic organisms, and can more clearly distinguish the time scale of paleoclimate and paleoenvironmental changes.

There are generally two types of lakes associated with volcanism, one is crater lakes and the other is dammed lakes. A crater lake is a lake formed by water in a crater, and a volcanic lake formed by a special type of closed crater is called Lake Marr.

This kind of lake is mostly round, with a diameter of 200-300 meters; The surrounding crater walls are generally a few meters to tens of meters high, with a relatively gentle top; The water of the lake is clear and calm, with a depth of several 10 meters. Zhanjiang Lake Guangyan is the most typical Mar Lake.

Formed by volcanic eruptions. You can take a look at the program Geography China for yourself, which talks about Lake Mar in China.

Legend has it that there was no lake in Huguangyan originally, and it was the location of two villages, Ning and Tuo. There is a mother and son in Ning Village who depend on each other, but unfortunately the son fell to his death while collecting firewood, and the old mother cried to death.

In the haze, she saw a little white cow who came to farm for her son, and from then on, grain grew in the field automatically. One year there was a great drought, and the white cow quietly brought food to the old mother's house.

The villagers found the white ox and slaughtered it and distributed it to the families to satisfy their hunger.

When the old mother found out, she cried bitterly and threw the beef back. Strange to say, the beef flew out of the village, the old mother stumbled after it, and a bamboo branch fell from the sky for her.

Chased to the edge of the mulberry field outside the village, the beef suddenly disappeared, and then thunder and lightning suddenly rose, and then the sky collapsed, and the village became Jiangze.

In a hurry, the old mother inserted bamboo branches into the field, and the thunder and lightning suddenly stopped, and the flood gradually receded, leaving a clear lake and mountain. This is today's Huguang Rock.

Of course, this is just a myth. However, it is not false to say that Huguang Rock was formed by the collapse of the sky and the earth. According to scientific research, it was formed by the lava eruption and depression 200,000 years ago.

Its birth process is more wonderful and magnificent than the myth portrays. Its mottled cliffs are the best testimony to the eruption. There are four volcanic lakes in China, among which Jingpo Lake and Wudalianchi are formed by lava blocking the river channel, called volcanic dammed lake, and only Changbai Mountain Tianchi and Huguangyan are crater lakes.

That's it, that's an easter egg, the reason why the ghost lake is cursed, it's a gimmick for players to build momentum, there are a few glowing stones by the lake, and it will light up at night, and then the lake is also quite special, that is, you drive into the car or something, you can't see it outside the lake. I think it's just because the lake is dirty.

Lake Mar is a volcanic eruption of the Mar type.

It is a kind of lake that is different from the crater lake. The English word for "maar" is in Latin.

"mare", which means sea, is the name given to the lakes and marshes that inhabit the Rhine region of Germany. In the early 19th century, the German scientist Steininger first recovered from the Quaternary period in the Eifel plateau in western Germany.

The study of the small, circular crater lake in the volcanic area began with the initial definition of maar as a volcanic type. In recent years, Buchel has conducted a comprehensive study of Mar in the Eifel region of western Germany, proposing that Mar is a system composed of ring walls, crater sediments, volcanic tubes, and slurry channels, and summarizing the different evolutionary stages of Mar's occurrence and development.

Zhanjiang Lake Guangyan is the starting point for the study of Lake Mar in China, and since 1996, the lake Guangyan has been listed in the National Natural Science of China**.

49772173] and the international "Eurasian Lake Mar" research program and other projects, and has achieved significant scientific research results.

Using a new generation of high-precision, non-disturbance drilling technology, the Quaternary lacustrine sediment samples with continuous and complete structure were successfully obtained from Tianyangyan Ranqing Mar Lake, and some research was carried out on paleoclimate and paleoenvironmental changes. According to numerous boreholes and studies of the relationship between volcanic rock chronology and stratigraphic contact, the Tianyang Mar Lake was formed after two phases of volcanic activity. The early volcanoes occurred in the Early Pleistocene, which generated Zhanjiang volcanic rocks, and erupted four times before and after, and formed a deep crater crater.

Late volcanoes occurred in the Middle Pleistocene (, generating rocks from Shiyiling volcanic rocks. Due to the mechanical mixing of high temperature (more than 1000) magma, hydrothermal fluid, vapor and water in the original crater, it has formed a typical Mar Lake, and has gone through five evolutionary stages: empty lake, deep lake, semi-deep lake, shallow lake, and swamp, and has become an important place for studying global change with its unique closure and special physical and chemical conditions.

In 1997, the United Nations Earth Research Center, together with experts from the Institute of Geology of the Zhongqi Academy of Sciences, spent 4.5 million US dollars to survey and control the lake rock, and from the analysis of the drilled sediment, it was determined that the lake rock is rare in the world and the only one in China. There are four main signs: (1) Groundwater breaks through the earth's surface and flats the earth.

2) ** when spewing water vapor and debris instead of magma. (3) The water level of the lake is below sea level. (4) Water is groundwater infiltrated from the ground, which does not dry up or overflow in drought.

After two years of research and analysis, scientists can analyze the changes in ancient typhoons, paleoclimate, and paleorainfall over the past 160,000 years on the entire earth. Understanding the rise and fall of human beings and the changes of plants on the whole earth provides an important scientific basis for the current protection of the earth's environment. It has attracted great attention from the United Nations and the Chinese Academy of Sciences.

Now, the new United Nations mission is to establish an environmental observation point in Huguangyan.