NCTF 135 HA Near Chessington, Surrey

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Location and Geography

NCTF 135 HA Background

Geography and Location

The National Cycle Track Facility (NCTF) 135 HA is situated near Chessington, which is a town in the county of Surrey, England.

Surrey is a part of the southeastern region of England, known for its scenic countryside and historic towns and cities.

Geographically, NCTF 135 HA can be found near the North Downs, a range of low-lying hills that stretch from Hampshire to Kent.

The area surrounding NCTF 135 HA is characterized by rolling hills, wooded areas, and open spaces, making it an attractive location for outdoor activities such as cycling and horse riding.

Chessington, where the facility is located, has a rich history dating back to the Bronze Age, with evidence of human habitation in the area from around 2000 BC.

The town’s name is derived from the Old English words ‘cecsa’ meaning ‘church’ and ‘ingtun’ meaning ‘settlement’, likely referring to a church or monastery that once stood in the area.

Climate

The climate in the region surrounding NCTF 135 HA is classified as temperate oceanic, with mild winters and cool summers.

The average temperature ranges from around 2-3°C (36-37°F) in January, which is the coldest month, to around 17-18°C (63-64°F) in July, which is the warmest month.

The area experiences a moderate amount of rainfall throughout the year, with an average annual rainfall of around 600 mm (24 in).

Topography

NCTF 135 HA is situated on relatively flat ground, with no significant elevation changes in the surrounding area.

The facility is surrounded by a mix of wooded areas and open spaces, providing a varied landscape for users to enjoy.

The North Downs, which are located nearby, offer a range of scenic views and opportunities for outdoor activities such as hiking and cycling.

Access

NCTF 135 HA is easily accessible by car or bike, with the A3(M) motorway and the M25 orbital motorway both within close proximity to the facility.

The nearest railway station is Chessington South, which is served by Southern trains and provides regular services to London Waterloo and other local towns and cities.

There are also a range of bus routes that serve the area, providing easy access to NCTF 135 HA for users who do not have a car or prefer to use public transport.

Environmental Factors

NCTF 135 HA is situated in an area of relatively high environmental quality, with minimal air pollution and no significant noise pollution sources nearby.

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The surrounding countryside provides a range of habitats for local wildlife, including birds, small mammals, and insects.

The facility’s location also provides opportunities for users to engage in outdoor activities that promote physical activity and mental well-being, such as cycling and horse riding.

The area of NCTF 135 HA is situated near Chessington in Surrey, England.

The area of NCTF 135 HA is situated in a picturesque part of England, specifically in the county of Surrey.

Located near the charming town of Chesterfield‘s neighbor, Che, Chessington is a notable district in south-west London. However, for geographical purposes, NCTF 135 HA can be considered as being situated in the county of Surrey rather than Greater London.

The geography of this area features rolling hills and gentle slopes, typical of the North Downs, which are an east-facing escarpment that forms part of the South East England Chalk Formation.

NCTF 135 HA is generally a low-lying area with some elevation variation throughout. The terrain includes areas of woodland and farmland, providing a mix of natural habitats for local wildlife and agricultural land use.

The NCTF 135 HA area receives an oceanic climate with significant rainfall throughout the year. Winters are typically mild but can be wet, while summers tend to be warm with occasional heatwaves.

The proximity of NCTF 135 HA to major roads and motorways makes it an easily accessible region for commuting or leisure activities in nearby London, Guildford, and other surrounding areas.

Its location near the River Mole adds further scenic beauty and ecological value to this area, supporting a diverse range of plant and animal species.

The NCTF 135 HA’s geographical features, including its rolling hills, woodland, farmland, and nearby watercourse, contribute to making it an attractive region for both residents and visitors alike.

Geological Features

Sandy Soil Composition

The geological features present in the area surrounding NCTF 135 HA near Chessington, Surrey, are primarily comprised of the Croydon and Purley Formations, which date back to the Eocene epoch, around 40-50 million years ago.

These formations are characterized by a complex mixture of sand, silt, and clay deposits that have been shaped over millions of years through a combination of fluvial, marine, and tectonic processes.

The Croydon Formation is primarily composed of soft to medium-hard grey to brown sandstones, silts, and clays, which were formed as a result of the deposition of sediments in a deltaic environment.

The Purley Formation, on the other hand, consists mainly of compact, fine-grained glauconitic sandstones and shales, which were deposited in a marine environment under relatively deep-water conditions.

The soil composition in this area is primarily sandy, with a high content of quartz sand grains. The presence of glauconite, a greenish-blue mineral, in the Purley Formation suggests that the area was once subjected to marine erosion and deposition.

The sand in this area is highly variable in terms of its particle size distribution, ranging from fine sands with particles less than 0.0625 mm in diameter to coarse sands with particles up to 2 mm in diameter.

The soil has a low silt content and a relatively high organic matter content, which suggests that it may be subject to seasonal variations in moisture levels.

These geological features and soil composition play an important role in shaping the local ecosystem and influencing the surrounding landscape. The complex mixture of sand, silt, and clay deposits has given rise to a diverse array of flora and fauna, while the presence of glauconite suggests that the area may be prone to marine erosion and deposition.

Understanding these geological features and soil composition is essential for managing the natural resources in this area and mitigating the impacts of climate change and other environmental factors on the local ecosystem.

The terrain within this region consists primarily of sandy soil, influenced by the presence of chalk beneath.

The area of NCTF 135 HA near Chessington, Surrey, boasts a unique geological profile that has been shaped by both natural and human-induced factors.

The terrain within this region primarily consists of sandy soil, which can be attributed to the underlying presence of chalk beneath the surface.

The chalk deposits in this area are part of the Chalk Group, a geological formation that dates back to the Late Cretaceous period, approximately 65-100 million years ago.

The chalk was originally deposited as the shells and skeletons of marine organisms such as plankton and algae, which accumulated on the sea floor over millions of years.

Over time, the pressure and heat caused these organic remains to compress into a solid, white limestone that is rich in calcium carbonate.

The chalk has played a significant role in shaping the local terrain due to its relatively soft and porous nature, making it susceptible to erosion by wind and water.

As a result, the chalk deposits have been worn away, leaving behind a landscape of sand dunes and valleys that are characteristic of this region.

The sandy soil found in NCTF 135 HA near Chessington is primarily composed of quartz grains, which were transported to the area through fluvial processes such as rivers and streams.

The quartz grains, along with other sedimentary particles like feldspar and mica, have been deposited on top of the chalk deposits over millions of years.

These sediments have been subjected to various weathering processes, including mechanical weathering (e.g., frost action), chemical weathering (e.g., hydrolysis), and biological weathering (e.g., root activity).

The combination of these factors has resulted in the formation of a complex network of valleys and hills within NCTF 135 HA near Chessington.

The terrain also exhibits various landforms, including dry valleys, sandy ridges, and small lakes that are remnants of glacial activity during the Pleistocene era.

Human activities have also impacted the geological features in this region through urban development, agriculture, and quarrying, which has further altered the landscape of NCTF 135 HA near Chessington.

Water Table and Drainage

The geological features present within the NCTF 135 HA near Chessington, Surrey are primarily composed of Cretaceous and Tertiary age deposits.

The area consists mainly of Upper Chalk (Cretaceous) overlain by Bracklesham Group (Eocene) and then topped with a thin layer of Bagshot Formation (Oligocene).

Geologically, the chalk is composed primarily of the calcareous skeletal remains of microscopic planktonic organisms that lived during the Cretaceous period.

The presence of flint nodules within the Chalk indicates periods of intense weathering and erosion in the distant geological past.

The Bracklesham Group consists mainly of sands and clays which were deposited in a coastal plain environment.

The Bagshot Formation is predominantly composed of clay and fine-grained sand, and was also deposited in a low-lying coastal area.

In terms of the water table within NCTF 135 HA near Chessington, Surrey, it’s difficult to determine an exact depth without specific hydrological data.

However, it can be suggested that the water table is likely situated at a depth below the surface where the pore space in the soil is fully saturated with water.

The local groundwater regime within the area would likely be influenced by precipitation, land use, and the underlying geology.

Drainage features present within NCTF 135 HA near Chessington, Surrey are primarily influenced by the topography and local geology.

As such, surface water flow within the area is primarily controlled by the gradient of the terrain and the presence of any artificial drainage structures.

The underlying geology likely plays a crucial role in determining groundwater movement and availability within NCTF 135 HA near Chessington, Surrey.

The chalk beneath the Bracklesham Group and Bagshot Formation is highly permeable due to its porous nature, allowing for significant groundwater flow.

The water table is generally shallow but can be subject to variation based on seasonal changes or specific geological conditions.

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The water table at NCTF 135 HA near Chessington, Surrey can exhibit significant variation due to seasonal changes and specific geological conditions.

One of the key factors influencing the water table in this area is the local geology.

• The region’s underlying strata comprise a mix of clay, silt, and sand deposits from various geological periods.
• The presence of these diverse sedimentary rocks plays a crucial role in determining groundwater levels.

Seasonal changes also impact the water table at NCTF 135 HA.

• In winter months, increased precipitation and higher groundwater recharge rates contribute to elevated water tables.
• In contrast, warmer summer periods often result in lower groundwater levels due to decreased rainfall and increased evapotranspiration from plants and soil.

Geological features within the area can also influence local variations in the water table.

• The presence of nearby chalk aquifers, which are characterized by their high permeability and significant groundwater storage capacity, can contribute to localized increases in groundwater levels.
• In contrast, areas with more impermeable geology, such as clay or hard rock formations, may experience lower groundwater levels due to reduced infiltration rates.

Furthermore, human activities within the NCTF 135 HA area can also impact local water tables.

• Groundwater abstraction for various purposes, including domestic and agricultural uses, can lower local groundwater levels.
• Conversely, infiltration of rainwater or artificial recharge systems designed to augment groundwater storage may elevate water tables in specific areas.

Understanding these factors is essential for managing the water resources within NCTF 135 HA near Chessington, Surrey effectively and ensuring sustainable development practices throughout the region.

Ecological Characteristics

Biodiversity and Wildlife Habitat

The National Cycle Track Facility (NCTF) 135 HA near Chessington, Surrey is a vast area that plays host to numerous ecological characteristics, biodiversity features and wildlife habitats.

Ecological Characteristics:

• This region has a temperate oceanic climate with mild winters and cool summers. The temperature range allows for a variety of flora to thrive within the area.

• The landscape is predominantly made up of heathland, which is a unique ecological habitat rich in biodiversity. Heathlands are characterized by acidic soils and an understory dominated by low-growing shrubs and wildflowers.

• There are numerous ponds scattered throughout the region, which provide a vital source of water for wildlife and help maintain the local hydrological balance.

Biodiversity Features:

• This area supports a wide variety of plant species. The heathland provides a home to many rare and endangered flora, including the Bee Orchid, and the Purple Milkweed.

• The region is also home to an assortment of mammal species, such as badgers, rabbits, hares and various bat species, which inhabit the area’s diverse habitats.

Wildlife Habitat:

• The NCTF 135 HA is a vital habitat for numerous bird species. The area’s ponds support aquatic birds like waterfowl, and its woodlands attract songbirds and raptors.

• In addition to the plant and animal diversity, this region also serves as an essential habitat for several invertebrate groups, including insects, arachnids and mollusks.

It is worth noting that while this area provides a wide range of ecological characteristics, biodiversity features and wildlife habitats, it’s equally important to recognize the potential human impact on these ecosystems. Therefore, conservation efforts are crucial for preserving the delicate balance between human activities and natural environments like NCTF 135 HA near Chessington, Surrey.

As an area near Chessington, NCTF 135 HA has the potential for various habitats such as woodland and grasslands hosting a range of local species.

The NCTF 135 HA area near Chessington in Surrey presents an environment with diverse ecological characteristics that support a variety of habitats and species.

Woodland Habitat:

• The woodlands within this region are comprised primarily of deciduous tree species, such as oak (Quercus robur) and ash (Fraxinus excelsior), which provide a complex structure for biodiversity.

• These woodlands also contain undergrowth featuring shrubs like dog rose (Rosa canina) and wild privet (Ligustrum vulgare).

• This diversity of vegetation supports a rich fauna, including woodland birds such as the great spotted woodpecker (Dendrocopos major), blue tit (Cyanistes caeruleus), and tawny owl (Strix aluco).

Grassland Habitat:

• The grasslands in this area are typically composed of a mixture of tall grasses, including meadow sweet (Filipendula ulmaria) and red fescue (Festuca rubra), alongside wildflowers like buttercups (Ranunculus acris) and knapweed (Centaurea nigra).

• These grasslands are often grazed by livestock, which maintains a mosaic of different habitats that support local species, such as skylark (Alauda arvensis), lapwing (Vanellus vanellus), and the common lizard (Lacerta vivipara).

NCTF 135 HA also hosts a range of aquatic habitats, including ponds and streams, which are critical for supporting local aquatic species such as amphibians like the natterjack toad (Epidalea calamita) and freshwater fish.