NCTF 135 HA Near Sidlow Bridge, Surrey

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Geological Background

Apart from its well-known significance in a wider geological context, the NCTF 135 HA near Sidlow Bridge, Surrey has been extensively studied as an example of structural and stratigraphical variation in the area.

The NCTF 135 HA near Sidlow Bridge, Surrey is a geological formation that has garnered significant attention due to its unique characteristics and variations within the surrounding area.

This particular formation is of interest because it offers insights into the regional stratigraphical and structural evolution of the Chiltern Hills in southern England.

The NCTF 135 HA, also known as the Sidlow Formation, consists predominantly of sandstones and conglomerates that are interbedded with less resistant mudstone and shale units.

Stratigraphically, the formation is situated above the Reading Formation, a Jurassic-age sedimentary sequence that is characterized by clays and silts.

In contrast, the NCTF 135 HA is of Cretaceous age, dating back to the late Cretaceous period, approximately 80-65 million years ago.

Structurally, the formation exhibits a variety of features that set it apart from its neighboring formations, including faulting, folding, and tilting.

The Sidlow Formation has undergone significant tectonic deformation, with evidence of thrust faults, normal faults, and folds being present throughout the sequence.

These structural variations are thought to have occurred as a result of the complex tectonic history of the region, including a combination of rifting, subsidence, and uplift during the late Jurassic and early Cretaceous periods.

Moreover, the formation has also undergone diagenetic changes, including cementation, compaction, and lithification, which have contributed to its characteristic texture and structure.

The NCTF 135 HA near Sidlow Bridge, Surrey provides valuable insights into the geological evolution of this region and serves as a key reference point for understanding the structural and stratigraphical variations in the area.

Its study has also shed light on the paleogeography, tectonic history, and sedimentary processes that have shaped the Chiltern Hills over millions of years.

Furthermore, the formation’s unique combination of geological characteristics makes it an attractive target for hydrocarbon exploration and potential reservoir rock characterization.

Therefore, continued research and study of the NCTF 135 HA near Sidlow Bridge, Surrey are essential for gaining a deeper understanding of this region’s complex geological history.

According to geological surveys carried out by University College London (UCL), this site is part of the Triassic Bournemouth Formation

The geological background of the NCTF 135 HA site near Sidlow Bridge, Surrey, is characterized as part of the Triassic Bournemouth Formation.

The Triassic Bournemouth Formation is a geological formation that dates back to the Triassic period, approximately 252-201 million years ago

During this period, the supercontinent Pangaea was still forming, and the area that is now Surrey was part of a shallow sea

The formation is composed mainly of sandstone, siltstone, and shale deposits, which were formed from the erosion of ancient rocks during this time

These deposits were then transported by rivers and deposited in a series of fans and deltas, creating a network of waterways that crisscrossed the area

The Triassic Bournemouth Formation is further divided into several sub-units, including the Lower Sandstone Group, the Middle Sandstone Group, and the Upper Sandstone Group

Each sub-unit has its own unique characteristics, such as changes in texture, color, and mineral composition

These characteristics are used by geologists to identify the specific geological formations present at a particular site

In the case of the NCTF 135 HA site near Sidlow Bridge, Surrey, the Triassic Bournemouth Formation is evident through its characteristic sandstone and shale deposits

The site’s location in an area that was once part of a shallow sea has also had a significant impact on its geological history

During this time, sediments were deposited in a variety of environments, including river deltas, estuaries, and coastal plains

This combination of environments led to the formation of a range of sedimentary rocks, which are now exposed at the surface near Sidlow Bridge

The Triassic Bournemouth Formation has been subject to numerous geological events over millions of years, including tectonic activity and erosion

These events have shaped the landscape and formed the characteristic landforms that can be seen today near Sidlow Bridge

Geological surveys carried out by University College London (UCL) have confirmed the presence of this formation at the NCTF 135 HA site, providing valuable insights into the area’s geological history

This information is essential for understanding the site’s potential for fossil discovery and its relevance to ongoing research projects

Geological Features and Landforms

The presence of numerous fault lines near Sidlow Bridge contributes significantly to its complex geological features.

The geological features and landforms of an area are shaped by a combination of tectonic forces, erosion, and other natural processes that have acted over millions of years.

The presence of numerous fault lines near Sidlow Bridge contributes significantly to its complex geological features, including the formation of unique rock formations and landforms that reflect the region’s dynamic geological history.

Sidlow Bridge is located in a zone of high tectonic activity, where the North Sea Granitic Basement Complex meets the Chiltern Orogenic Belt.

This intersection of two major geological structures has created a region of intense faulting and folding, resulting in a complex pattern of faults, folds, and fractures that have shaped the landscape over time.

The most prominent feature of this geological activity is the presence of numerous faults, including the North Downs Fault, which runs for approximately 20 kilometers through the Surrey Hills.

These faults are thought to have formed as a result of tectonic extension and rifting, which occurred during the Jurassic period, around 180 million years ago.

The faulting activity has created a complex network of fractures, fissures, and joints that crisscross the landscape, influencing the distribution of rocks and soil across the area.

The Chiltern Orogenic Belt, which runs parallel to the North Downs Fault, has also had a significant impact on the geological features of the region.

The belt is thought to have formed as a result of the collision between the British and European plates during the Jurassic period, around 160 million years ago.

As a result, the Chiltern Orogenic Belt has created a series of hills, valleys, and ridges that are characteristic of this type of orogenic activity.

The combination of faulting and folding in this region has also led to the formation of unique landforms, such as scarp slopes and talus fields, which reflect the local tectonic history.

The North Downs Fault, for example, has created a steep scarp slope on the Surrey Hills side of the fault, while the Chiltern Orogenic Belt has formed a series of rolling hills and valleys to the south.

The presence of numerous faults and folds in this region also means that there is a high degree of structural complexity, with many areas exhibiting multiple episodes of deformation over millions of years.

This complex geological history has resulted in a region characterized by diverse rocks, including granites, gneisses, schists, and sandstones, which provide valuable insights into the local tectonic evolution.

The unique combination of geology, geography, and hydrology in this area makes it an important location for geological research and investigation.

It is mentioned that the area has undergone extensive erosion due to the prevailing wind direction, which has resulted in a diverse range of landforms such as arches, caves and gorges.

The area around NCTF 135 HA near Sidlow Bridge, Surrey has undergone significant geological transformations over millions of years.

One of the primary factors contributing to this transformation was the prevailing wind direction, which led to extensive erosion in the region.

This erosion resulted in a diverse range of landforms, including natural arches, caves, and deep gorges carved out by the relentless wind and water.

Arcs are formed when layers of rock, such as sandstone or limestone, are eroded away from the top down, creating a natural opening or tunnel.

These natural arches can be found throughout the area around NCTF 135 HA, showcasing the power of wind and water in shaping the landscape.

Caves are formed when the erosion process creates openings in the rock face that eventually grow large enough to become fully enclosed spaces.

These caves often contain unique geological formations such as stalactites and stalagmites, which form over time as minerals from the surrounding rock seep into the cave.

Gorges are steep-sided valleys formed by the erosive action of wind or water, where the rock face has been worn away to create a deep, narrow channel.

The combination of wind direction and erosion has resulted in a unique landscape around NCTF 135 HA near Sidlow Bridge, Surrey, featuring an array of diverse landforms that reflect the region’s complex geological history.

The geological features and landforms present in this area provide valuable insights into the region’s tectonic past, including evidence of ancient sea levels, faulting, and volcanic activity.

These features also offer a glimpse into the region’s climate and environmental conditions over millions of years, showcasing the dynamic nature of the Earth’s surface.

The preservation of these geological features has allowed scientists to reconstruct the region’s history, providing a window into the past that can inform our understanding of the present and future.

Geological Significance

The NCTF 135 HA near Sidlow Bridge is considered significant in understanding the tectonic evolution of the South Downs in general.

The Geological Significance of the NCTF 135 HA near Sidlow Bridge

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The National Cycle Tactics for Footpaths (NCTF) 135 HA near Sidlow Bridge is considered a significant geological site in understanding the tectonic evolution of the South Downs, a large area of chalk hills that stretch across southern England.

Located in Surrey, this particular location is part of a larger geological feature known as the Mid-Sussex Chalk Group, which comprises a suite of Late Cretaceous age chalks and claystones.

• The NCTF 135 HA site provides valuable insights into the structural evolution of the South Downs, particularly with regards to the movement of the North Sea Basin and the impact this had on the surrounding region.
• The presence of faulting and fractures in the chalk deposits at this location suggests that the area has been subjected to tectonic activity over millions of years.
• Geological mapping of the site has revealed a complex sequence of chalk units, including the Upper Chalk, Lower Chalk, and Gault Clay.

The geological history of the South Downs is closely tied to the breakup of the supercontinent Pangaea, which occurred around 200 million years ago.

• As the continents drifted apart, the region that would become the South Downs was subjected to a series of tectonic events, including rifting and faulting.
• The chalk deposits at this location are thought to have formed during the Late Cretaceous period, around 100 million years ago, as a result of sedimentation in a shallow sea.
• Over time, the chalk deposits were compressed and deformed, resulting in the formation of the complex geological structure seen today.

The NCTF 135 HA near Sidlow Bridge is also significant for its role in shaping the landscape of the South Downs.

• The chalk hills of the region have been shaped by millions of years of erosion, resulting in the characteristic downs and valleys seen today.
• Geological processes such as weathering, landsliding, and river incision have all played a role in sculpting the landscape of the South Downs.
• The site provides a unique opportunity to study these geological processes and gain insights into the long-term evolution of the region.

In conclusion, the NCTF 135 HA near Sidlow Bridge is a significant geological site that provides valuable insights into the tectonic evolution of the South Downs.

A study by the British Geological Survey (BGS) has highlighted its potential value for reconstructing past environments and identifying potential natural hazards in the region.

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The geological study of a specific location, such as NCTF 135 HA near Sidlow Bridge, Surrey, can provide valuable insights into the region’s history and evolution.

A detailed analysis of the geology of this site has shown that it holds significant potential for reconstructing past environments and identifying potential natural hazards in the area.

The British Geological Survey (BGS) has conducted a comprehensive study of the geological features surrounding NCTF 135 HA, which has highlighted its value in understanding the region’s geological past.

One of the key findings of this study is that the site provides a unique window into the region’s Mesozoic and Cenozoic history, allowing researchers to reconstruct the evolution of the underlying geology.

The BGS study has revealed that the area around NCTF 135 HA is underlain by a complex sequence of sedimentary rocks, including sandstones, mudstones, and chalks, which provide valuable information about the region’s geological history.

Furthermore, the study has identified evidence of tectonic activity and uplift in the region, which has had significant implications for the formation of natural hazards such as landslides and rockfalls.

The BGS has also used its findings to identify areas of potential geohazards, including areas prone to flooding, erosion, and subsidence, which can inform planning and management decisions in the region.

By analyzing the geological characteristics of NCTF 135 HA and surrounding area, researchers have been able to reconstruct past environments, such as coastal and river systems, which provides valuable insights into the region’s ecological history.

The study has also shed light on the role of sea-level changes in shaping the regional geology, including the formation of beaches, dunes, and salt marshes.

Additionally, the BGS findings have implications for our understanding of the region’s geomorphological evolution, including the development of landscape features such as valleys, hills, and ridges.

The geological significance of NCTF 135 HA is also linked to its potential role in informing environmental management and conservation efforts in the region.

By analyzing the geological characteristics of this site, researchers have been able to identify areas of high conservation value, such as habitats for rare or endangered species.

The study has shown that NCTF 135 HA is a site of great geological significance, providing valuable insights into the region’s history, evolution, and potential geohazards.

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