Danxia landform is formed by the combined effect of volcanic activity and geological movement, and its most notable feature is the sight of strange peaks and rocks.

These landforms are primarily sandstone and mudstone, deposited millions of years ago in river deltas and basins.

Over time, these sedimentary rocks underwent intense tectonic activity, including folding, faulting, and uplifting, leading to their uplift and exposure.

One of the distinguishing features of Danxia landforms is their vibrant red and orange colors.

These colors result from a complex chemical called hematite or iron oxide oxidation. The iron-rich minerals in the sandstone and mudstone undergo weathering, allowing iron oxide minerals to form.

When exposed to the elements, these minerals react with oxygen in the air, giving rise to the vivid hues that characterize Danxia formations.

Another prominent feature of Danxia landforms is their unique shapes and patterns.

These formations often exhibit a combination of sharp peaks, deep valleys, and intricate ridges, resulting in a captivating landscape.

The distinctive shapes are mainly a result of erosion and weathering processes acting on the softer layers of the rock formations. Water, wind, and gravity play significant roles in gradually sculpting the landforms over millions of years.

Rainfall and river runoff carve deep channels and gorges into the soft sedimentary rocks, creating a network of valleys.

The erosive power of water is further enhanced by the presence of multiple layers with varying hardness in the rock formations, leading to vertical cliffs and steep slopes.

Strong winds carry fine sediments and abrasive particles, which gradually wear away the exposed rocks, smoothing their surfaces and creating unique features such as alcoves, arches, and caves.

Over time, wind erosion can cause intricate patterns and formations to emerge, adding to the visual appeal of these landscapes.

The climatic conditions prevailing in the regions where Danxia landforms are found also contribute to their formation.

The combination of a subtropical monsoon climate and frequent rainfall provides ample moisture necessary for chemical weathering and erosive processes.

The alternating wet and dry seasons, with periods of heavy rainfall followed by prolonged droughts, further contribute to the mechanical weathering and disintegration of the rocks.

At the same time, the volcano's eruption also provides an important material basis for forming landforms in the Danxia area, which produce magma and lava experience the role of natural physical processes and the formation of special strata.

The development process of the Danxia area has experienced volcanic activity, weathering and erosion, collapse, and other links after billions of years of evolution.

Danxia landform is one of the unique landscape wonders of the earth, and the uniqueness of its natural form and the complexity of its genesis mechanism make people more enthusiastic about studying and exploring its geomorphological significance and value.