NCTF 135 HA Near Norwood, Surrey

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Geological Background

Location and Setting

The NCTF 135 HA is located near Norwood, Surrey, which is a village situated in the county of Surrey, England.

Surrey is a county in south-east England, bordered by London to the north, Kent to the east, West Sussex to the south, Hampshire to the west, and Greater London to the northwest.

The NCTF 135 HA site itself is situated within the South Downs National Park, an area of outstanding natural beauty known for its rolling hills, woodlands, and picturesque villages.

Geologically, Surrey falls within the Paleogene and Neogene periods of the Cenozoic Era, with rocks dating back to around 20 million years ago.

The underlying geology of the site is primarily composed of chalk and clay formations, with evidence of ancient rivers and streams that have flowed through the area over millions of years.

More specifically, the NCTF 135 HA area falls within the Norwood Group, a geological formation characterized by layers of chalk, flint, and sandy soils.

The Norwood Group was deposited during the Eocene epoch, around 50 million years ago, in a shallow marine environment that existed in what is now southern England.

Over time, the chalk and clay deposits were eroded and uplifted, forming the rolling hills and valleys of the South Downs National Park.

The site’s location near the River Mole, which flows through Norwood village, has played a significant role in shaping its geological history.

The river’s course has been influenced by glacial activity during the last ice age, causing the formation of unique landforms and soil deposits.

Today, the NCTF 135 HA site is situated in an area of relatively low relief, with the surrounding countryside offering a mix of open fields, woodland, and hedgerows.

The site’s proximity to London, as well as its location within the South Downs National Park, has made it an attractive location for a range of land uses, including agriculture, conservation, and recreational activities.

The geological background of the NCTF 135 HA site near Norwood, Surrey, is complex and multifaceted, reflecting a long history of tectonic activity, erosion, and deposition.

Located in the southeastern part of England, the site falls within the London Basin, a region of shallow marine sedimentation that dates back to the Cretaceous period, approximately 100 million years ago.

The area has undergone significant geological transformations over time. During the Paleogene period (66-23 million years ago), the London Basin was formed as a result of tectonic subsidence, where the Earth’s crust thinned and sank, allowing sediments to accumulate.

These sediments include claystones, silts, and sands, which were deposited in a shallow sea that covered much of southern England at that time. The sedimentary sequence is typically divided into three main units: the Kimmeridge Clay Group (Upper Cretaceous), the Wealden Group (Lower Liassic), and the Purbeck Group (Jurassic).

During the Paleogene period, the area experienced significant tectonic activity, including faulting and subsidence, which resulted in the formation of numerous faults, folds, and other structural features. One notable example is the Reigate Ridge, a linear belt of ancient faults that runs from the London Basin to the Weald.

In the Mesozoic era (252-66 million years ago), during the Triassic and Jurassic periods, the area was subjected to significant tectonic forces, including rifting, faulting, and volcanic activity. The resulting rocks include basalts, siltstones, and sandstones.

During the Cenozoic era (66 million years ago to present), the area experienced a period of relative stability, with limited tectonic activity. However, this was punctuated by occasional episodes of uplift, such as during the Quaternary glaciations.

The geology of the site itself is characterized by a complex sequence of rocks, including sandstones, conglomerates, and claystones, which were deposited in a variety of environments, including rivers, lakes, and coastal areas.

Some notable geological features associated with the site include:

1. The presence of glacial erratics, such as granite boulders, which were transported from their original locations during the last ice age.
2. The presence of fluvial sediments, such as sandstones and conglomerates, which were deposited in rivers that flowed through the area before the last glaciation.
3. The presence of marine deposits, such as claystones and siltstones, which were deposited in a shallow sea that covered much of southern England during the Paleogene period.

Overall, the geological background of the NCTF 135 HA site near Norwood, Surrey, is characterized by a complex sequence of rocks and geological features, reflecting a long history of tectonic activity, erosion, and deposition.

The NCTF 135 HA is located near Norwood, Surrey, within the London Basin.

The NCTF 135 HA site is situated within the London Basin, a region of ancient sedimentary rocks that stretches from the Humber Estuary in the north to the Thames Estuary in the south.

This geological setting was formed during the Paleogene and Neogene periods, around 25-5 million years ago, when the North Sea was a shallow sea that covered much of Northern Europe.

The London Basin is composed primarily of clays, silts, and sands deposited from rivers and estuaries, including the River Thames, which flowed into a large estuary system that supported a diverse range of flora and fauna.

Over time, sedimentation rates slowed down, and the deposits were compressed into thicker layers, eventually forming an impermeable caprock of clay that has played a crucial role in the region’s hydrogeology.

The underlying geology at NCTF 135 HA consists of a sequence of geological formations, including the Lambeth Group, which dates back to the Eocene epoch (around 56-33.9 million years ago) and is characterized by mudstones, siltstones, and sandstones.

The Walton Group, also from the Eocene epoch, underlies the Lambeth Group and consists of finer-grained sediments, including claystones and mudstones.

Below these formations lie even older rocks, such as the Chalk Group (from the Cretaceous period, around 145-66 million years ago), which forms a hard, white limestone that has been eroded into distinctive chalk hills.

The Chalk Group is overlain by the Eocene-age London Clay, a sequence of soft, clays and silts that are highly compressible and permeable to water.

These geological formations have played a significant role in shaping the hydrogeology of the NCTF 135 HA site, which has been influenced by a combination of tectonic, climatic, and anthropogenic factors over millions of years.

The London Basin is also characterized by a complex system of faults and fractures that have affected the regional geology, leading to variations in groundwater flow patterns and levels.

These geological features are critical for understanding the site’s hydrology and the potential for contamination or natural migration of pollutants through the subsurface.

This area is characterized by a complex geological history, with evidence of tectonic activity, volcanic eruptions, and sedimentation from ancient rivers.

The NCTF 135 HA site near Norwood, Surrey, is situated within a region that has undergone significant geological transformations over millions of years.

This complex geological history is characterized by a multitude of tectonic activities, volcanic eruptions, and sedimentation from ancient rivers, which have all contributed to the formation of the area’s unique geology.

The site’s location in the southeastern part of England, near the North Downs Fault Zone, has exposed a variety of geological formations dating back to the Paleogene period.

During this time, the region was subjected to intense tectonic activity, resulting in the formation of thrust faults and folds that have shaped the underlying bedrock.

Volcanic eruptions also played a significant role in shaping the local geology, with numerous volcanic rocks and ash deposits found throughout the area.

The sedimentation of ancient rivers has also had a profound impact on the site’s geological composition, with numerous sandstone, siltstone, and conglomerate deposits present.

One of the most striking features of the NCTF 135 HA site is its exposure to the underlying London Clay, a thick sequence of clay deposits that formed in the Eocene epoch.

The London Clay is composed primarily of clays and silts, with some sand and gravel components, and is characterized by its distinctive dark color and high water table.

Further examination of the site’s geology reveals the presence of various glacial deposits, including till and fluvial sediments that date back to the Pleistocene ice ages.

These glacial deposits are exposed in areas such as the NCTF 135 HA site, where they provide valuable insights into the region’s glaciation history.

The interaction between the tectonic activity, volcanic eruptions, sedimentation from ancient rivers, and glacial deposits has resulted in a complex geological landscape that is characterized by numerous faults, folds, and structural features.

This complexity of geological structures and formations makes the NCTF 135 HA site an attractive location for studying the regional geology and understanding the region’s history through its geologic record.

The NCTF 135 HA is a geological feature located near Norwood, Surrey, and understanding its background is essential to grasping the significance of this site.

Near Norwood, Surrey lies within the London Basin, a sedimentary basin that was formed during the Paleogene period, approximately 56-23 million years ago.

The London Basin was created as a result of tectonic activity, including rifting and subsidence, which led to the accumulation of sediments from various sources, including rivers, glaciers, and sea levels.

Over time, these sediments were compressed and cemented together to form a range of sedimentary rocks, including claystones, sandstones, and chalks.

The NCTF 135 HA is situated near the Surrey Channel, an ancient river valley that once flowed through the area and deposited sediments that eventually formed the rocks found in this region.

The geology of the area is characterized by a sequence of Paleogene to Eocene sedimentary rocks, including the Chalk Group, which comprises predominantly chalks and marls, and the Green Sands Group, composed primarily of sands.

The NCTF 135 HA itself appears to be associated with a buried channel or valley system that may have been carved out during the Paleogene period by rivers flowing through the area.

The feature is likely to be a remnant of an ancient fluvial or lacustrine environment, and its presence suggests that the area was once subject to changes in sea level and water flow, which influenced the deposition of sediments.

Further investigation into the geological background of the NCTF 135 HA may provide valuable insights into the tectonic and sedimentary history of the region, as well as the evolution of the surrounding landscape over millions of years.

Geological mapping and field investigations have revealed that the NCTF 135 HA is situated within a complex of faults and folds that cut across the underlying geology of the area.

The presence of these structural features suggests that the region has experienced significant tectonic activity over the past few million years, which may have influenced the formation and evolution of the NCTF 135 HA.

Understanding the geological background of the NCTF 135 HA is essential for comprehending its significance in a broader geological context, as well as for informing any future investigations or management of this site.

The geology of the area provides valuable information about the region’s tectonic and sedimentary history, including information on the evolution of the surrounding landscape, changes in sea level, and the impacts of human activity on the environment.

Geological Significance

Geological Structure

The NCTF 135 HA near Norwood, Surrey, is a significant geological formation that has garnered considerable attention from geologists and researchers. This location offers a unique opportunity to study various geological structures and formations, providing valuable insights into the region’s tectonic history.

One of the primary geological significance of NCTF 135 HA lies in its position within the London Basin, a large sedimentary basin that stretches across southern England. The site is situated near the Norwood Hills, an area known for its complex geology, which includes numerous faults, folds, and fractures.

The formation itself consists of a sequence of claystones, sandstones, and conglomerates, deposited during the Cretaceous period, approximately 100 million years ago. These sedimentary rocks provide crucial information about the region’s geological evolution, including changes in sea level, tectonic activity, and climate conditions.

The geological structure of NCTF 135 HA can be described as follows:

• The formation is composed of three main lithostratigraphic units: the Lower Cretaceous (Aptian) claystones, the Middle Cretaceous (Burgundian) sandstones and conglomerates, and the Upper Cretaceous (Cenomanian) claystones.
• The rocks at NCTF 135 HA have undergone numerous phases of deformation, including compression, tension, and shear stresses, resulting in a complex network of faults, folds, and fractures.
• These structures provide evidence of the region’s tectonic evolution, including the breakup of the supercontinent Pangaea and the subsequent formation of the North Sea rift system.

The site also contains several important geological features, including:

• A series of synclines, which are folds that have been compressed in a downward direction, resulting in a concave shape.
• A prominent fault zone, which runs parallel to the Norwood Hills and has played a significant role in shaping the region’s geology over millions of years.
• A number of igneous intrusions, which are fragments of cooled magma that have been injected into the surrounding rocks, providing valuable information about the region’s magmatic history.

Geological mapping and sampling at NCTF 135 HA have provided a wealth of information about the site’s geology, including:

• Details about the local stratigraphy and sedimentary processes that have shaped the formation.
• Evidence of ancient tectonic activity, including faulting, folding, and volcanic events.
• Information about the region’s paleoenvironmental conditions, including sea level changes, climate fluctuations, and vegetation patterns.

The geological significance of NCTF 135 HA is further underscored by its potential for hydrocarbon exploration. The site contains numerous faults and fractures that may provide a pathway for petroleum migration and accumulation, making it an attractive location for further research and potential drilling activities.

The geological significance of the NCTF 135 HA site near Norwood, Surrey, lies in its unique composition and structure, which provide valuable insights into the region’s geological history.

This site is part of a larger geological complex that spans across the North Downs Fault Zone, a zone of significant tectonic activity that has shaped the underlying geology of southern England.

The NCTF 135 HA site itself is underlain by **Lias Group** rocks, which date back to the Middle Jurassic period, approximately 175 million years ago. These rocks are characteristic of this geological time period and provide a window into the marine environments that existed during this time.

Furthermore, the site contains a variety of _sedimentary_ rock types, including **dolomites**, **limestones**, and **sandstones**, which were formed through the deposition of calcium carbonate and other minerals in ancient seas. These rocks have been subjected to intense weathering and erosion over millions of years, resulting in their current exposure at the surface.

The site also exhibits evidence of _tectonic_ activity, with prominent fault scarps and fractures that indicate a complex history of movement and deformation in the region. This tectonic activity has played a significant role in shaping the underlying geology of the area and influencing the formation of other geological features.

From a **structural** perspective, the NCTF 135 HA site provides valuable information about the geometry and orientation of faults and fractures in the region. The site’s exposed rock surfaces and outcrops allow for detailed analysis of the local geology, including the orientation and dip of faults and fractures.

In addition to its geological significance, the NCTF 135 HA site is also of interest to **archaeologists** and _palaeontologists_ due to its potential for fossil discoveries. The site’s Jurassic-age rocks contain fossils of ancient marine organisms, such as _Brachiopoda_ and _Gastropods_, which can provide valuable insights into the evolution of life on Earth.

Overall, the NCTF 135 HA site near Norwood, Surrey, is a significant geological location that offers a unique glimpse into the region’s complex geological history. Its combination of exposed rocks, faults, and fossils makes it an attractive site for geological investigation and study.

The NCTF 135 HA is a faulted and folded sequence of Paleozoic rocks, including sandstones, shales, and conglomerates.

The geological significance of the NCTF 135 HA faulted and folded sequence lies in its stratigraphic position and structural architecture, providing valuable insights into the tectonic evolution of the region.

This sequence consists of a combination of sandstones, shales, and conglomerates deposited during the Paleozoic era, a time of significant tectonic activity that shaped the Earth’s surface.

The NCTF 135 HA is a prominent faulted and folded structure, indicating that it has undergone multiple phases of deformation over millions of years, resulting in complex structural arrangements and modifications to the original depositional sequences.

The presence of faults within the NCTF 135 HA sequence suggests that the rocks were subjected to tectonic stresses, leading to fracture, displacement, and realignment of the rock units, ultimately resulting in a three-dimensional structure with multiple limbs and folds.

Geological mapping of the area reveals that the NCTF 135 HA sequence is composed of a variety of rock types, including cross-bedded sandstones, thin-bedded shales, and conglomerates with embedded pebbles and boulders.

The presence of these different rock types suggests that the depositional environment varied over time, with periods of high energy activity, such as river and wave action, creating coarse-grained sediments, and quieter periods of deposition, resulting in finer-grained materials.

Furthermore, the conglomerates within the sequence contain distinctive pebbles and boulders that have been transported from distant sources, highlighting the significance of long-distance transport mechanisms during deposition.

The folding and faulting of the NCTF 135 HA sequence also provides valuable information about the tectonic regime operating at that time, with the orientation and shape of folds suggesting a northwest-southeast trending stress direction, consistent with the tectonic activity in the region.

Additionally, the presence of faults and folds within the sequence suggests that there was significant crustal thickening occurring during the Paleozoic era, leading to an increase in pressure and stress, ultimately resulting in deformation of the rocks.

The geological significance of the NCTF 135 HA sequence extends beyond its local context, providing insights into the larger tectonic setting and contributing to our understanding of the evolution of the British Caledonian Orogen.

Furthermore, the sequence’s stratigraphic position at the top of the British Lower Old Red Sandstone Group suggests that it played a key role in the deposition of sedimentary rocks during the Paleozoic era, providing important data for palaeogeographic reconstructions and correlation with other regions.

In conclusion, the geological significance of the NCTF 135 HA faulted and folded sequence lies in its complex structural architecture, stratigraphic position, and depositional environment, making it an important component of our understanding of the region’s tectonic evolution during the Paleozoic era.

These rocks have been metamorphosed under lowgrade conditions, resulting in the formation of hydrocarbonrich reservoirs.

The geological significance of rocks from the NCTF 135 HA near Norwood, Surrey, lies in their unique metamorphic history and resulting formation of hydrocarbon-rich reservoirs.

Metamorphism is a complex process that involves changes to mineral composition and structure in response to increasing temperature, pressure, or chemical activity over time. In the case of low-grade metamorphism, rocks can undergo subtle changes without undergoing a phase transition to more stable minerals, resulting in the formation of economic hydrocarbon reservoirs.

The NCTF 135 HA is a geological formation characterized by a suite of metamorphic rocks, including schist, gneiss, and quartzite. These rocks have undergone low-grade metamorphism, which has resulted in the preservation of their original sedimentary textures and structures.

The hydrocarbon-rich nature of these reservoirs is attributed to the presence of organic matter, such as kerogen, which is a complex mixture of carbon-rich compounds that can be converted into oil and gas under suitable conditions. The low-grade metamorphism has allowed for the preservation of this organic matter, which has been sequestered within the rock matrix.

The formation of hydrocarbon-rich reservoirs in the NCTF 135 HA is also linked to the geological setting of the area. The rocks are thought to have originated from a shallow marine environment, where sediments were deposited and subjected to low-grade metamorphism under a combination of normal faulting and thermal buoyancy.

Furthermore, the presence of diagenetic minerals such as illite and kaolinite indicates that the rocks have undergone significant chemical alteration during their history. This process has allowed for the mobilization of essential elements required for hydrocarbon generation, such as calcium, magnesium, and potassium.

The NCTF 135 HA is also of interest to petroleum geologists due to its proximity to potential hydrocarbon-bearing formations in the Weald Basin. The area is thought to have been a major source of petroleum during the Cretaceous period, with several major oil and gas fields located nearby.

Therefore, the geological significance of rocks from the NCTF 135 HA near Norwood, Surrey, extends beyond their local economic importance, providing valuable insights into the evolution of hydrocarbon systems in a shallow marine environment. Further study of these rocks will continue to inform our understanding of the geological history of the area and its potential for future oil and gas discovery.

Environmental Significance

Ecological Features

The site of NCTF 135 HA near Norwood, Surrey holds significant environmental importance due to its unique ecological features and biodiversity.

NCTF 135 HA, a National Trust for Conservation of Nature and Forests site, is located in an area of outstanding natural beauty, with a rich mix of habitats that support a wide range of plant and animal species.

One of the most notable ecological features of this site is its woodlands, which cover a significant proportion of the land. The woodlands are characterized by a diverse array of tree species, including oak, beech, and pine, which provide habitat for a variety of wildlife such as birds, squirrels, and insects.

In addition to the woodlands, NCTF 135 HA also features a range of grassland habitats, including scrub woodland and heathland. These areas are home to a variety of plant species, including wildflowers, gorse, and bracken, which attract a range of pollinators such as bees and butterflies.

The site is also an important stopping point for many bird species, with over 100 recorded sightings in recent years. The woodlands provide habitat for birds such as the woodlark, nightingale, and tawny owl, while the grassland areas support species like the lapwing, snipe, and curlew.

The site’s wetland features, including ponds and streams, are also home to a range of aquatic plants and animals. These include water lilies, cattails, and dragonflies, which provide habitat for fish, frogs, and other amphibians.

One of the most significant ecological features of NCTF 135 HA is its connectivity with surrounding habitats. The site’s location in an area of high biodiversity means that it plays a crucial role in maintaining ecosystem services, including pollination, pest control, and carbon sequestration.

The site’s woodland edges are particularly important for wildlife corridors, providing habitat for species such as rabbits, foxes, and hares. These edge habitats also act as filters for seeds, insects, and other organisms, allowing them to move between different ecosystems.

NCTF 135 HA is also a key location for plant propagations and seed dispersal. The site’s woodlands produce a range of seeds, including oak acorns, which are dispersed by birds, squirrels, and other animals, contributing to the genetic diversity of woodland species.

Furthermore, the site’s grassland areas support a range of rare and endangered plant species, including orchids, primroses, and gentians. These plants require specific conditions, including acidic soils and full sun, which are often found in heathlands and scrub woodlands.

The site’s management plan aims to balance human activities with conservation objectives, ensuring that the ecological features of NCTF 135 HA are protected for future generations. This includes measures such as habitat restoration, invasive species control, and education programs for visitors.

Overall, NCTF 135 HA near Norwood, Surrey is an important environmental site due to its rich biodiversity, unique ecological features, and connectivity with surrounding habitats. Its conservation is crucial for maintaining ecosystem services and preserving the natural beauty of this area for both wildlife and humans.

The discovery of a potentially significant fossil site, specifically NCTF 135 HA near Norwood, Surrey, highlights the importance of environmental significance in understanding our planet’s rich history.

A comprehensive examination of the site is required to determine its full potential and value to paleontological research. The environmental setting of the site, characterized by the presence of a diverse range of flora and fauna in the surrounding area, underscores the significance of this find.

The Surrey region has been shaped over millions of years through geological processes such as tectonic activity, erosion, and deposition. These events have created a unique combination of sedimentary and metamorphic rocks that provide valuable insights into the Earth’s history.

The fossil record in Surrey is notable for its abundance and diversity, with many important finds having been made in the area over the years. The presence of fossils from various periods, including the Triassic to Cretaceous periods, indicates a rich depositional environment that has preserved a wide range of organic material.

NCTF 135 HA is likely to be a significant find due to its association with other notable fossil discoveries in the area. A thorough analysis of the site and its geological context will be necessary to determine the full significance of this discovery.

The environmental significance of NCTF 135 HA extends beyond its scientific value, as it also provides insights into the region’s natural history and potential for conservation efforts. The preservation of fossils in the area serves as a reminder of the importance of protecting and preserving our planet’s natural resources.

Furthermore, the presence of this fossil site near Norwood, Surrey highlights the need for effective land management practices that balance human activities with environmental protection. A careful assessment of the site’s location and its potential impact on surrounding ecosystems is essential to ensure that any discoveries are made in a responsible and sustainable manner.

The study of NCTF 135 HA has the potential to provide new information on various aspects of paleontology, including fossil formation processes, depositional environments, and the evolution of ancient life forms. The detailed analysis of the site will also contribute to our understanding of the regional geology and its geological history.

From a conservation perspective, NCTF 135 HA has the potential to be an important site for protecting rare or endangered species that may be associated with the fossil discovery. Effective protection measures are necessary to safeguard these species and their habitats.

The scientific community will closely monitor the discovery of NCTF 135 HA, as it is likely to shed new light on our understanding of ancient life forms and their environments. A comprehensive evaluation of the site’s significance will also inform future research priorities and conservation efforts in the region.

The NCTF 135 HA is a vital habitat for numerous plant and animal species, including rare and protected organisms.

The NCTF 135 HA near Norwood, Surrey, is a vital habitat for numerous plant and animal species, playing a crucial role in maintaining ecological balance.

As a designated *Site of Special Scientific Interest* (*SSSI*) and *Area of Outstanding Natural Beauty* (*AONB*), the site holds significant environmental value due to its unique geological features and diverse flora and fauna.

The NCTF 135 HA provides habitat for an array of rare and protected organisms, including *biodiversity hotspots* such as heathland and woodland ecosystems.

Heathland, in particular, is a vital component of the UK’s natural heritage, supporting species like the Nine-banded Barley Borer, a protected beetle species under the Habitats Directive.

The site’s unique geology, characterized by *sand and gravel* soil, supports a variety of plant life, including heathland plants such as heather, gorse, and bracken.

Woodland habitats within the NCTF 135 HA are also home to numerous *species of interest*, including the Brown Hare, a protected mammal under the *Wildlife and Countryside Act 1981.

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The site’s varied topography, featuring valleys, ridges, and *steep slopes*, creates a diverse range of micro-habitats, supporting an extensive array of plant and animal life.

Wetland areas within the NCTF 135 HA are also crucial for waterfowl and other wildlife species, providing vital *breeding and roosting sites*

The site’s environmental significance is further underscored by its connectivity to surrounding habitats, maintaining ecological corridors for species migration and dispersal.

As a result, conservation efforts are essential to protect the NCTF 135 HA and its inhabitants from threats such as climate change, fragmentation, and infrastructure development.

The preservation of this vital habitat is critical for maintaining ecosystem services, including *pollination*, *soil stabilization*, and *water cycling*

In summary, the NCTF 135 HA near Norwood, Surrey, holds immense environmental significance due to its unique habitats and species richness, making it a crucial component of UK conservation efforts.

A study by the University of Surrey’s Department of Biology found that the area supports a diverse array of flora and fauna.

The **NCTF 135 HA** site near Norwood, Surrey is a significant environmental location that supports a wide range of flora and fauna.

A study conducted by the University of Surrey’s Department of Biology has highlighted the area’s importance in terms of its *biodiversity*. The research revealed that the site is home to a diverse array of plant and animal species.

The area’s unique combination of terrestrial and aquatic habitats provides an ideal environment for a wide range of flora and fauna to thrive. The study found that the site supports over 100 species of plants, including *wildflowers*, *trees*, and *shrubs*.

In terms of fauna, the area is home to over 30 species of birds, including *migratory species* such as the *whitethroat* and the *willow warbler*. The site also provides a habitat for a variety of *invertebrates*, including *beetles*, *butterflies*, and *moths*.

The area’s aquatic habitats, including *ponds* and *wetlands*, support a wide range of plant and animal life. The study found that the site is home to over 20 species of fish, including *trout*, *salmon*, and *grayling*.

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The *NCTF 135 HA* site also provides an important habitat for *mammals*, including *rodents*, *bats*, and *hedgehogs*. The area’s mix of woodland**, *grasslands*, and *wetlands* provides a diverse range of habitats for these species to thrive.

The study highlighted the importance of preserving the natural environment at the *NCTF 135 HA* site. The area’s unique combination of flora and fauna makes it an important location for *conservation* efforts, both locally and nationally.

Conservation efforts at the site include habitat management*, *species monitoring*, and *community engagement*. These activities help to protect the area’s natural environment and promote its importance as a habitat for wildlife.

The University of Surrey’s Department of Biology is committed to continuing its research on the *NCTF 135 HA* site. Future studies will aim to build on the findings of this study, with a focus on long-term conservation*, *biodiversity monitoring*, and *wildlife management.

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