Why did the Lower Triassic spring form?

The Lower Triassic Spring is located in Lushan Scenic Area, which benefits from geological structure, climate and topography. Abundant precipitation and mountain rock fissures provide channels for groundwater flow, groundwater in the surface of the formation of springs, outflow to form springs. Spring clear, sweet, contains a variety of minerals beneficial to the human body. Its formation process has the characteristics of unique geological structure, sufficient water supply and long underground flow time.

I. Geographical location and geological background

The Lower Triassic Spring is located in the Lushan Mountain Scenic Area of Jiujiang City, Jiangxi Province, close to the South Bank of the middle and lower reaches of the Yangtze River. Carries a geological history of about 200 million years ago, belonging to the Jurassic Period.

Lushan unique geological structure, after hundreds of millions of years of wind and rain baptism, formed a unique landscape, the Lower Triassic spring as part of Lushan, Has also witnessed the vicissitudes of this land.

Lower Triassic Spring is located in Lushan Scenic Area, surrounded by mountains, landscapes blend, pleasant scenery, tourists have come here, To see the magic of nature.

In the ancient land of Lushan Mountain, the Lower Triassic spring with its unique geological background, has become the yearning of many tourists.

I. Geographical location and geological background

The geological structure is intricate, and numerous geological movements have shaped the rich geological remains of the land, the area where the Lower Triassic springs are located, To limestone and sandstone-based, constitute its unique geological structure.

Spring from the geological structure, its formation and the nature of the rocks here are inseparable, for this piece of land has brought vitality and vitality.

In the baptism of time, these geological formations have become a masterpiece of nature, attracting the attention of countless explorers.

The Lower Triassic spring is located in a high mountain, its water source from rain and snowmelt, through the surface infiltration into the rock crevices.

Spring flow process, rock cracks continue to expand, forming springs of different sizes.

With the evolution of geological structure, springs continue to erode rocks, creating a unique spring scenery.

Climatic factors such as rainfall and temperature affect the flow and quality of spring water.

Topography such as mountain trend and soil type play a key role in spring flow path and landscape formation.

Natural conditions for the formation of springs

Lushan region has a unique climate, belongs to the subtropical humid climate, abundant annual precipitation, which laid a solid foundation for the formation of springs.

Abundant rainfall, making the mountain rocks fully absorb water, through underground infiltration, converged into clear springs.

The special rock structure of Lushan Mountain is easy for groundwater infiltration and accumulation, which is also an important reason for the continuous emergence of spring water.

Mount Lushan, peaks, rolling mountains, mountain rocks between the cracks, as the labyrinth of nature.

These fissures, like countless small rivers, provide a path for the flow of groundwater.

In this winding path, groundwater through the rocks, gathered into a trickle, and finally formed the clear sweet spring water.

Process of spring formation

Groundwater flows slowly deep underground. When it meets a crack in the rock, it seeps quietly and converges into a clear spring. This clear spring in the geothermal and pressure of the dual role, slowly gushing out of the surface, forming a spring.

Spring in the underground flow process, constantly absorbing the nutrients of the stratum, making the water clear and sweet, rich in a variety of minerals beneficial to the human body.

Spring gushes out from the spring, flows into the river, nourishes the surrounding ecological environment, becomes the precious resources which the nature gives us.

Spring in the flow process, but also constantly in contact with the ground, making the spring water become warm and moist, become an indispensable part of people's lives.

Process of spring formation

The spring meanders underground, touching the rocks along the way.

Minerals in rocks, such as calcium, are dissolved by spring water.

These minerals blend with the spring water, giving it a unique flavor and color.

Spring Surging, from the depths of the earth, a clear spring after geothermal and pressure of the double honed, and finally break through the surface, gushing out of the ground, Into a series of gorgeous scenes.

Spring, as if nature carefully carved jade liquid qiongjiang, continuously, forming a unique landscape - the Lower Triassic spring.

Spring gurgling, reflecting the blue sky and white clouds, nourish all things on the earth, has become a beautiful landscape on this land.

In the long river of time, spring water constantly flowing, telling the magic of nature and beauty, intoxicating among them, linger.

Uniqueness of spring water formation

The Lower Triassic spring water is clear and rich in many kinds of minerals beneficial to human body.

Spring from the depths of the underground, through the filter of rock, with years of precipitation, slowly flowing, in the sun, sparkling, Like a string of Crystal clear pearls.

Spring along the way through the jungle, nourishing the surrounding vegetation, making this land full of vitality and vitality, its unique formation process, Not only for people to provide a precious drinking water, but also become a treasure given to humanity by nature.

Uniqueness of spring water formation

Lushan Spring, like a heaven-sent treasure, its formation process is unique, hundreds of millions of years of geological changes, shaping a unique rock structure, Rock fissures crisscross, providing an ideal flow path for groundwater.

Deep groundwater flowing slowly in the rock fissures, full contact with minerals, water quality can be constantly purified, and gradually formed the sweet and pure Lushan spring.

More Lushan Spring in the geographical location, so that it can fully absorb the essence of heaven and earth, fresh air, the sun through the leaves sprinkled mottled light and shadow, Injected the vitality of life into the spring.

It is these unique geological structure and natural environment, given the Lushan spring unique quality, making it a natural drink that people are fascinated by.

Uniqueness of spring water formation

Spring Surging in the depths of the earth, gathering the essence of the earth, its formation process unique.

Spring water supply is sufficient, relying on abundant rainfall, continue to gush, as the source of life.

Each drop of spring carries a natural rhythm, they shuttle between the rock crevices, giving birth to a unique spring scenery.

Spring formed in the rock cracks, after a long period of infiltration and circulation, only to gushing out.

Uniqueness of spring water formation

Spring slowly flowing underground, time flies, its close contact with the rock, so that minerals gradually dissolved in the flow, into which.

After a long time, spring water in the depths of the underground, quietly pregnant with a unique quality, carrying the gift of the earth.

In this long journey, the blend of spring and rock, not only gives the spring rich minerals, but also makes it a rare resource in the world.

Every drop of spring water, are carrying the secrets of nature, telling the legend of the millennium.

Where is the Lower Triassic spring
The Lower Triassic Spring is located in Lushan Mountain Scenic Area of Jiujiang City, Jiangxi Province, close to the South Bank of the middle and lower reaches of the Yangtze River. Carrying about 200 million years of geological history, belonging to the Jurassic Period, the Lower Triassic spring as part of Lushan, also witnessed the vicissitudes of the land.
What is the geological background of the Lower Triassic spring
Lower Triassic Spring is located in Lushan Scenic Area, surrounded by mountains, landscape blend, pleasant scenery, Lushan Unique Geological Structure, after hundreds of millions of years of wind and rain baptism, Formed a unique geomorphologic landscape, the Lower Triassic spring in the region, mainly limestone and sandstone, constitute its unique geological structure, Spring from the geological structure, its formation and the nature of the rocks here are inseparable, for this piece of land has brought vitality and life.
Where does the water source of the Lower Triassic spring come from
The Lower Triassic spring is located in a high mountain. Its water source comes from rain and melting snow. The formation of springs of different sizes, with the evolution of geological structure, springs continue to erode rocks, creating a unique spring landscape, Climatic factors such as rainfall and temperature affect the flow and quality of springs. Topography such as mountain trend and soil type play a key role in spring flow path and landscape formation.
What is the formation process of the Lower Triassic spring
Groundwater flows slowly deep underground. When it meets a crack in the rock, it seeps quietly and converges into a clear spring. This spring in the geothermal and pressure under the dual role, slowly gushing out of the surface, forming a spring, spring water in the underground flow process, Constantly absorbing the nutrients of the strata, making the water clear and sweet, rich in a variety of minerals beneficial to the human body, springs gushing from the spring, Into the river, nourish the surrounding ecological environment, nature has become a valuable resource for us.