NCTF 135 HA Near Holmwood, Surrey

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Geological Formation

Nature of NCTF 135 HA Deposit

The NCTF 135 HA deposit located near Holmwood, Surrey, is a complex geological formation that has garnered significant interest due to its unique characteristics and potential industrial applications.

Nature of the Deposit: The NCTF 135 HA deposit is composed primarily of kaolin, a type of clay mineral that is rich in alumina and silica. This deposit is believed to have originated from the weathering of granite rocks, which were then transported and deposited through various geological processes.

Geological Setting: The NCTF 135 HA deposit is situated within the Wealden Clay Formation, a geologically significant unit that spans parts of southern England. This formation is characterized by a series of clay deposits, including kaolin, which were formed as a result of weathering and erosion.

Geological Processes: The NCTF 135 HA deposit has been shaped by a range of geological processes, including tectonism, weathering, erosion, and deposition. These processes have worked in concert to concentrate the kaolin deposits and create the complex structure that characterizes this site.

Mineralogy: The NCTF 135 HA deposit is notable for its high concentration of kaolinite, a type of clay mineral that is prized for its industrial applications. Additionally, the deposit contains smaller amounts of other minerals, including quartz, feldspar, and mica.

Potential Applications: The NCTF 135 HA deposit has significant potential applications in a range of industries, including paper production, ceramics, and refractory materials. Its high-quality kaolin deposits make it an attractive source material for these industries.

Conclusion: In conclusion, the NCTF 135 HA deposit near Holmwood, Surrey, is a complex geological formation that has been shaped by a range of geological processes. Its high-quality kaolin deposits and diverse mineralogy make it an important industrial resource with significant potential applications.

The NCTF 135 HA near Holmwood, Surrey is a geological formation primarily composed of sand, with minor amounts of gravel.

The Geological Formation of NCTF 135 HA near Holmwood, Surrey is a significant and complex geological site that offers valuable insights into the region’s geological history.

The primary component of this formation is sand, which forms the majority of the deposit. The sand in this area is characterized as being fine to medium-grained, with an abundance of quartz grains. The presence of quartz is not surprising given its common occurrence in many sedimentary formations.

In addition to the dominant sand content, minor amounts of gravel are also present throughout the formation. Gravel, a coarser aggregate than sand, contributes to the site’s complex stratigraphy and adds to our understanding of the depositional processes that shaped this area over millions of years.

From a geological perspective, NCTF 135 HA near Holmwood, Surrey can be interpreted as a sedimentary deposit laid down in a fluvial or alluvial environment. The presence of sand and gravel suggests that these sediments were transported by water from the surrounding hillslopes and deposited in a low-lying area during periods of high runoff.

Further analysis of this formation reveals evidence of lithic weathering, where rocks have undergone chemical alteration due to exposure to acidic soil conditions. This type of weathering is typical for areas with moderate to high levels of rainfall, which is consistent with the regional climate in Surrey.

The stratigraphic sequence of NCTF 135 HA near Holmwood, Surrey also provides a valuable record of past environmental changes and geological events. The presence of distinctive sedimentary features such as cross-bedding and channel fills offers insights into the dynamics of the ancient rivers that deposited these sediments.

It belongs to the Bagshot Beds formation, a Cenozoic deposit that formed as part of the London Basin.

The geological formation at NCTF 135 HA near Holmwood, Surrey, is part of the Bagshot Beds, a Cenozoic deposit that formed as part of the London Basin.

The London Basin is a large sedimentary basin located in southeastern England, which was created during the Cenozoic era due to tectonic uplift and erosion of older rocks.

The Bagshot Beds are a geological formation that dates back to the Paleogene period, around 58-56 million years ago, during the late Eocene epoch.

They are a type of sandstone and clay deposit that were formed as a result of rivers flowing through the area, carrying sediments and depositing them in the basin.

The Bagshot Beds are composed mainly of sand, silt, and clay minerals, with some limestone and other minor components.

They have a distinctive red or orange color due to the presence of iron oxide and other minerals that were introduced during their formation or later alteration processes.

The Bagshot Beds are an important part of the London Basin’s geological history, providing valuable information about the region’s tectonic evolution, climate conditions, and paleo-environmental changes.

They have also been used as a source of building materials for many years, with the sandstone and clay being quarried for use in construction and other applications.

The NCTF 135 HA site near Holmwood is likely to be part of this Bagshot Beds formation, which would give it significant geological importance and potential for further study and research.

This particular deposit is likely to be an aeolianite or eolianite.

The geological formation at NCTF 135 HA near Holmwood, Surrey is of great interest and can be attributed to various factors that led to its creation. As per the given information, this particular deposit is likely to be an aeolianite or eolianite.

Aeolianites are a type of sedimentary rock that forms through the accumulation and cementation of sand grains deposited by wind. These deposits typically occur in arid or semi-arid regions where there is significant wind activity, allowing for the transportation and deposition of sand particles over time.

The aeolianite formation at NCTF 135 HA can be attributed to the Cretaceous period, a geological era characterized by significant aridity in many parts of the world. During this time, vast deserts stretched across Europe, Africa, and Asia, providing an ideal environment for wind-blown sand deposits.

The Cretaceous period is also associated with the breakup of supercontinents, resulting in the formation of new coastlines and sea levels that fluctuated significantly over time. This led to the creation of numerous marine basins where aeolianites could form through the accumulation of sand deposited by wind from adjacent deserts.

The specific location of NCTF 135 HA near Holmwood, Surrey suggests that this deposit is likely part of a larger eolianite sequence in southern England. This region has been known to have significant aeolian deposits formed during various geological periods, with some dating back to the Mesozoic era.

The geological characteristics of NCTF 135 HA, such as its composition and bedding patterns, are also consistent with those found in other eolianites across southern England. These features include well-defined cross-bedding, prominent grain size variations, and an overall uniformity that can be attributed to the slow and steady process of wind-blown sand deposition.

Additionally, the location near Holmwood, Surrey suggests that this deposit may have formed in a coastal environment where the action of waves, tides, and currents helped shape the eolianite over time. This is supported by observations of similar deposits found along southern England’s coastline, which often exhibit signs of marine modification.

Further research on NCTF 135 HA, such as detailed sedimentary analysis, geochronological dating, and microfossil identification, would provide valuable insights into its formation and the geological history of the area. By understanding this unique deposit, scientists can gain a deeper appreciation for the complex processes that shaped our planet’s surface over millions of years.

Geologists and researchers will be able to make more informed decisions about how to conserve and manage these deposits as they are considered significant resources in reconstructing ancient landscapes and ecosystems.

Location and Surroundings

Topographical Context

The location of NCTF 135 HA is situated in the county of Surrey, a region known for its picturesque countryside and rolling hills.

The site lies near the village of Holmwood, which is a small settlement nestled in the heart of the Sussex Weald.

Topographically, the area can be characterized as part of the Wealden Axis, a geological formation that stretches from East Grinstead to Dorking and includes areas such as Leith Hill and Holmbury Hill.

The region is predominantly composed of Cretaceous chalk and gault, which have been eroded over time, resulting in a landscape of low hills and valleys.

The proximity to the North Downs to the south and the Greensand Ridge to the north indicates that NCTF 135 HA lies within an area of gentle hills and slopes, which has been shaped by millions of years of tectonic activity and weathering.

The North Downs, a chain of hills stretching from Farnham in Surrey to Box Hill in Surrey, is a prominent topographical feature visible from NCTF 135 HA, while the Greensand Ridge to the north marks the boundary between the Wealden Axis and the Chiltern Hills.

The landscape surrounding NCTF 135 HA has been shaped by glacial activity during the Devensian, which resulted in the formation of numerous valleys and ridges.

The site is situated on a gentle slope, with an elevation of around 80-100 meters above sea level, providing panoramic views of the surrounding countryside.

The local geology is characterized by a mixture of Chalk, Gault, and Purbeck Limestone, which have been exposed through erosion and weathering over millions of years.

NCTF 135 HA lies within an area of rich biodiversity, with numerous species of flora and fauna present in the surrounding landscape.

The site’s location near Holmwood provides access to a network of footpaths and bridleways, allowing for exploration of the surrounding countryside on foot or by horseback.

The NCTF 135 HA near Holmwood, Surrey sits within a lowlying area in the Wealden Hills.

The NCTF 135 HA near Holmwood, Surrey, is situated within a low-lying area of the Wealden Hills, a picturesque and historic region in southern England.

The Wealden Hills, often referred to as the ‘Low Weald’, are part of a larger area known for its rolling hills, woodlands, and valleys, formed by ancient river systems and erosion over millions of years.

This specific location is nestled in a valley, which provides a relatively flat terrain compared to the surrounding hills, creating a tranquil atmosphere that is characteristic of many parts of the Wealden region.

The geography of this area has been shaped by human activity as well, with historical records showing extensive forestry and agricultural practices, including charcoal burning and wood pasture management in the past, which have contributed to its current landscape features.

From a hydrological perspective, the NCTF 135 HA near Holmwood, Surrey, is part of the River Mole catchment area. The Mole River flows through the Wealden Hills before eventually joining the Thames River.

The region’s natural surroundings are rich in biodiversity, with common plant species including oak, ash, and beech trees, as well as various wildflowers, grasses, and ferns that thrive in the milder climate of southern England.

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Local wildlife includes a variety of bird species, mammals, such as deer, hares, and foxes, and insects like butterflies and dragonflies, which contribute to the area’s ecological health and beauty.

The NCTF 135 HA near Holmwood, Surrey, sits within close proximity to several footpaths and nature trails that traverse this region, making it an excellent base for outdoor explorations, including walking, cycling, or horse riding through the Wealden Hills.

Holmwood itself is nestled within the Mole Valley, which is part of the larger North Downs.

The location of NCTF 135 HA near Holmwood, Surrey, provides a picturesque and serene setting for outdoor activities and exploration.

Located in the Mole Valley, Holmwood is surrounded by rolling hills, woodlands, and scenic countryside views.

Here are some notable features of the location:

• The North Downs: The area surrounding Holmwood forms part of the larger North Downs, a range of chalk hills that stretch from Surrey to Kent.

• Mole Valley: This is the specific valley in which Holmwood is nestled. It is characterized by its rolling hills and scenic countryside views.

The surroundings offer ample opportunities for outdoor recreation, including walking, hiking, and cycling through the picturesque countryside.

Visitors to NCTF 135 HA near Holmwood can enjoy the natural beauty of the area while participating in a range of activities and events.

The location provides a unique combination of scenic views, outdoor recreational opportunities, and educational experiences for individuals and groups.

This location places it within the Wealden anticline.

The location of NCTF 135 HA near Holmwood, Surrey places it within a specific geological region known as the Wealden anticline.

The Wealden anticline is an important feature in the geology of southern England and is characterized by a series of folds and faults that have created a distinctive landscape.

The anticline is formed from a combination of Cretaceous and Jurassic rocks, which have been subjected to intense folding and faulting over millions of years.

The area around NCTF 135 HA near Holmwood, Surrey is dominated by **Weald Clay**, a type of soft, blue-grey clay that is characteristic of the Wealden anticline.

**Weald Clay** is an important source of building materials and has been extensively quarried in the past for use in construction.

In addition to Weald Clay, the area around NCTF 135 HA near Holmwood, Surrey also features other geological formations, including:

1. Reigate Stone: a type of limestone that is found in the area and has been used extensively for building purposes.
2. Copthorne Beds: a type of sandstone that is found in the area and is characterized by its distinctive orange-red color.

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The location’s proximity to the Wealden anticline also means that it is susceptible to various types of landslip, including clay slips and rock falls.

The Wealden anticline has been shaped over millions of years by a combination of geological processes, including weathering, erosion, and tectonic activity.

The area around NCTF 135 HA near Holmwood, Surrey features a mix of woodland, heathland, and arable land, which provide a range of habitats for local wildlife.

The Wealden anticline is also an important area for geology-related tourism, with many visitors drawn to the region’s distinctive landscape and geological features.