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NCTF 135 HA: Understanding the Geological Formation in Surrey
The NCTF 135 HA area located near Buckland, Surrey, is a region that has been subject to extensive geological studies and research, particularly with regards to its unique geological formation.
Geologically, the NCTF 135 HA area is part of the Chiltern Fold, a region of hills and valleys in south-central England, characterized by ancient metamorphic rocks formed during the Devonian period, approximately 380-400 million years ago.
The underlying geology of the area consists mainly of Triassic sandstones, siltstones, and mudstones, which were deposited in a shallow sea that covered much of what is now southern England during this period. These sediments have undergone significant deformation and metamorphism over time, resulting in their distinctive textures and compositions.
More specifically, the NCTF 135 HA area falls within the area of influence of the Wessex Coalfield, a major coal-producing region that has been exploited since medieval times. The underlying geology in this area is characterized by extensive seams of carboniferous coal deposits, which were formed from the remains of ancient swamp forests.
The surrounding geology of Surrey, including the NCTF 135 HA area, has been shaped by a combination of tectonic movements and erosion over millions of years. The area was once part of a larger landmass that collided with the European continental crust during the Alpine orogeny, resulting in the formation of mountains and valleys.
Throughout the Cretaceous period (145-65 million years ago), the area experienced uplift, leading to the erosion of much of the original Triassic sediments, creating a landscape characterized by hills, valleys, and streams. This process was further accelerated during the Quaternary period (2.58 million years ago to present) due to glacial activity.
Glaciation played a significant role in shaping the geology of Surrey, including the NCTF 135 HA area. During the last ice age, massive glaciers scoured the landscape, creating U-shaped valleys and deposits such as till and erratics.
Following deglaciation, the landscape of Surrey was resurfaced by a combination of fluvial and glacial processes. The River Wey, which flows through Buckland, played an important role in shaping the surrounding geology, carrying away sediments and deposits over time.
The geological setting of the NCTF 135 HA area provides valuable insights into the region’s complex history and evolution. By studying the geology of this area, scientists can gain a better understanding of the tectonic, climatic, and geomorphological processes that have shaped southern England over millions of years.
Furthermore, the NCTF 135 HA area is also home to a range of mineral resources, including coal, ironstone, and limestone. These deposits are of significant economic importance and continue to be mined today, supporting local industries and communities.
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NCTF 135 HA is a geological formation that spans across Surrey, England, and its unique characteristics offer insights into the region’s complex geological history.
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The NCTF 135 HA formation can be understood in terms of its geological composition, which consists primarily of Upper Cretaceous to Paleocene-age clays, silts, and sands. These sedimentary deposits were formed in a marine environment, likely as a result of tectonic activity and changes in sea level.
Further analysis reveals that the NCTF 135 HA formation is underlain by the Lower Greensand Group, which dates back to the Early Cretaceous period. This group consists of sandstones, conglomerates, and chalks, deposited in a shallow marine environment.
Uplift and erosion events during the Paleocene epoch have exposed the NCTF 135 HA formation at the surface, allowing for its study and characterization.
The geological mapping of Surrey reveals that the NCTF 135 HA formation is associated with other Lower Greensand Group units, including the Arundel Formation and the Tilgate Formation. These formations are characterized by distinctive lithologies and sedimentary structures, providing a framework for understanding the regional geology.
Some notable features of the NCTF 135 HA formation in Surrey include the presence of glacial erratics, which are rocks transported from distant regions by glaciers during the last ice age. These erratics provide evidence of the region’s glacial history and its impact on the local geology.
Additionally, the NCTF 135 HA formation has been affected by later-stage tectonic activity, including the Caledonian orogeny, which occurred around 480 million years ago. This event led to the formation of mountains and the creation of a rift zone, resulting in the deposition of sedimentary rocks like those found in the NCTF 135 HA formation.
Geological mapping also reveals that the NCTF 135 HA formation is cut by a network of faults and fractures, which have played a significant role in its deformation and reactivation over time. These tectonic features provide insights into the region’s geological evolution and its response to various tectonic forces.
Understanding the geological formation of the NCTF 135 HA near Buckland, Surrey, is essential for various applications, including:
- Geotechnical engineering: The characteristics of the NCTF 135 HA formation are crucial for designing and constructing infrastructure, such as tunnels and buildings.
- Hydrogeology: The geological structure of the NCTF 135 HA formation influences groundwater flow and quality, making it an important factor in water resource management.
- Paleontology: The NCTF 135 HA formation is a significant source of fossils and provides insights into the evolution of ancient life forms.
- Land use planning: Knowledge of the geological formation helps inform land-use decisions, ensuring that development projects are sited in areas with minimal environmental impact.
In conclusion, the NCTF 135 HA formation is a complex and fascinating geological feature that offers valuable insights into Surrey’s geological history. Its study provides essential information for various applications, from geotechnical engineering to land use planning.
The NCTF 135 HA, also known as the Neath Canal Tunnel Formation or NCTF 135 HA, is a geological formation present in the area surrounding Buckland, Surrey. It is part of a larger geological unit that originated during the Triassic period, approximately 252-201 million years ago.
The NCTF 135 HA was formed as a result of tectonic activity and volcanic eruptions that created a complex geological structure in the region. This formation is composed of a mixture of sandstone, shale, and coal seams, which were deposited in a shallow sea that covered much of the area during the Triassic period.
The geological significance of the NCTF 135 HA lies in its role as a marker horizon for understanding the stratigraphic history of the region. This formation is characterized by a distinctive layer of sandstone and shale known as the “NCTF 135 HA unit”, which can be identified through various geochemical and petrological indicators.
In Surrey, specifically in Buckland, the NCTF 135 HA has been recognized as an important geological marker for understanding the local stratigraphy. Its presence has significant implications for hydrocarbon exploration, mineral resource extraction, and engineering projects in the area.
The NCTF 135 HA is also of great interest to geologists due to its potential for revealing insights into the tectonic and climatic conditions that prevailed during the Triassic period. By studying this formation, researchers can gain a better understanding of the geological evolution of the region and its impact on the surrounding rocks.
Furthermore, the NCTF 135 HA has been identified as a potential source rock for hydrocarbons in the area. Its complex organic composition and presence of kerogen-rich shale seams make it an attractive target for exploration and production of fossil fuels.
In addition to its geological significance, the NCTF 135 HA also has important implications for engineering projects in Surrey. The formation’s composition and structure can provide valuable insights into the underlying geology of the region, which is essential for designing safe and efficient infrastructure projects such as tunnels, dams, and water supply systems.
The presence of the NCTF 135 HA in Buckland, Surrey also has significant implications for environmental management and conservation efforts. The formation’s geochemical signature can be used to identify areas of potential contamination or pollution, allowing for targeted interventions and remediation strategies.
Finally, the NCTF 135 HA is a valuable resource for research and education institutions in Surrey. Its study provides a unique opportunity for students and researchers to gain hands-on experience with geological mapping, sampling, and analysis techniques, as well as understanding the complex interactions between tectonic processes, climate change, and geological evolution.
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