River Thames

 

Factfile

  • Length: 346 km

  • Sources: Thames Head (the cotswolds)

  • Key Tributaries: leach

  • Basin area: 12,935 km^2

  • Counties within: Gloucestershire, Wiltshire, Oxfordshire, Berkshire, Buckinghamshire, Surrey, Kent, Essex 

  • Basin Population: 14 million 

  • Discharge: 65.8 m³/s

 
Course of the RIver Thames

Course of the RIver Thames

Physical Geography

The Thames river is not one of the largest rivers in the world only spanning a length of 346 km, however there is a large amount of history in this region showing the relationship with humans and the fluvial environment. Below we will analyse the physical characteristics of the River Thames to understand how this system developed, throughout the large historical record of human occupation in this region.

Formation/Geology

The River Thames is a fluvial system that can date its origins to between 170 and 140 million years ago during the Jurassic period, when the region was submerged by the sea, with the formation of the limestone that would act as the building blocks of the system. This limestone would form the base for the Cotswold Hills where the source of the Thames is located. As the early seas regressed leaving much clearer water many organisms moved into the region including corals and mollusks, with their shells, with these species being the basis for the chalklands that are found within the basin.

Approximately 40 million years ago the seas of the region receded leading to the land that had been formed over millions of years emerging. The Thames would begin to gradually develop over the next 37-38 million years until the much larger Proto-Thames would form a tributary to what is the current Rhine, with a course that would have flowed more northward than its current setting. This connection with the rhine continued until the last ice age, which occurred 110,000 years ago, with the encroaching ice moving southward along the British Isles forcing the course of the Thames further south to a similar setting to that of the current Thames.

At this point the Thames continued to flow on a more southward course eroding the London Clay valley creating a series of geomorphological landforms including gravel and sand terraces along the course of the river. This vertical erosive behavior continued until the end of the last ice age, sea levels beginning to rise with the release of large volumes of water that was previously locked within the glaciers that had formed. With the increase in sea level, the erosive nature of the Thames changed, reducing the formation of the terraces that had been formed with the vertical erosion of the river leading to the current setting of the Thames.

Geomorphology

The course of the Thames can be broken down into three sections the Upper, Middle & Lower course in these regions the geomorphology of the river changes greatly. The Upper course of the Thames is located within the Cotswolds in this region the river Thames drains a broadly triangular area outlined by the chalk ridges of the Cotswolds, Chiltern Hills, Berkshire Downs and the Northamptonshire uplands. In this region the river eroded its way through the sedimentary rock of the region forming the Goring Gap, a narrow valley that is occupied by the Thames. Following the Goring Gap the Thames moves into its middle course with gently flowing lowlands with minimal change occurring in the elevation of the river, with a drop in elevation of 32 cm/km until reaching London. Once the river enters London it enters its lower course, with the Thames transitioning from a freshwater to estuarine environment around Battersea. Following this point the Thames becomes an estuary that is dominated by the tides of the north sea, where the mouth of the Thames is found, with a tidal range that can lead to an increase in 7 metres during spring tides and 5.5 metres during neap tides. As a result of the threats of sea-level rise leading to an increase in the amount of flooding along the banks of the Thames in the centre of London, the Thames Barrier was constructed allowing for the regulation of the Thames waterway itself, this however does prevent the some of the natural processes of the river including the deposition of fluvial sediments.

 
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Climate

The Thames basin is much smaller than relative to the other rivers in this series, as such the climate across the entirety of the basin is much more uniform. The climate of the basin can be described as a Maritime climate, much like the rest of the U.K, with mild summers and cool to cold winters. The Thames basin is located within one of the driest regions of the U.K. with an average annual precipitation of 690 mm while the average for the entirety of the U.K. is approximately 885 mm. The temperature across the basin is also mild, as described by the maritime climate, with an average summer temperature of 23°C with an average winter temperature of 5°C while freezing temperatures are not uncommon in the basin.

Ecosystems

The Thames river basin is a region that is mainly rural with around 17% of the entire basin area being categorised as urbanised, with much of the remaining 83% accounting for arable land, grassland and woodland, with large agricultural efforts. The presence of anthropogenic actions in this region for thousands of years has greatly impacted the ecosystem in the region leading to its current setting. 

Flora

Many of the Flora associated with the Thames are situated along the lowland course of the river and can be identified in other lowland ecosystems of the U.K.. However, there are two plants that are found in the basin that are unique to the region these are the Snake’s head Fritillary, located in the upper Thames, and the Loddon Lily a species of Summer Snowflake that is situated along the banks of the River Loddon a tributary of the Thames. Other common species that are identified in the region are Marsh Orchid, Dandelions, Buttercups, Ragged Robin, Meadowsweet, Great Burnet and Quaking grass. Many of the trees in the Thames basin are of three main species with Alders and Willows being situated along the banks while Beech trees dominate the woodlands of the catchment. Species of riparian and river based vegetation are quite infrequently found within the basin as a result of the anthropogenic dredging efforts for transportation means along the river’s course.

Fauna

The Fauna within the Thames basin has been studied for a long period of time providing a great overview of the many species of invertebrates, crustaceans, mammals, fish, and birds within the catchment. As such below the species found in the basin will be sub-categorised in order to develop an understanding of the many species that are found in the basin

Invertebrates 

  • Brown shrimp, Opossum Shrimp, Prawns, Oligochaete Worms, Ragworms, Shore crabs, and Chinese mitten crabs (an invasive species)

Insect

  • Alderfly, Mayfly, Caddisfly, Dragonfly, Damselfly, Pond skater

  • Water Hog-louse, River Limpet, Snail, Hermit crab, Cockles, Starfish and Whiteweed

Fish: Within the Thames there are some 120 identified species of fish including 2 species endemic to the region the Twaite Shad and Sea Lamprey, with spawning regions located within the tidal range of the Thames Estuary. Other species that are located along the course of the Thames include:

  • Roach, Chub, Perch, Pike, Bream, Dace, Barbel, Carp, Smelt, Sand Goby and Salmon

Birds

  • Mute Swan, Canada Goose, Mallard Duck, Greylag Goose, Great Crested Grebe, Coot, Grey heron, Moorhen

Mammals: in terms of mammals that are located in the catchment, most are small mammals that create their habitats close to the banks of the thames. Due to Anthropogenic actions over thousands of years other larger Mammalian species are not found in the wild throughout the Thames catchment.

  • Water Vole, Otter, American Mink

Human Geography

Modern urbanisation has been occurring throughout the Thames basin for hundreds of years since the beginning of the Industrial Revolution in the 18th century, however, a large human population has been situated within the boundary of the Thames basin for thousands of years since the Roman occupation of the British Isles. As such anthropogenic actions have been impacting the Thames for a long period of time, influencing the natural function of the region and affecting the Ecosystems and services that a natural environment provides. Agricultural practices are also very common throughout the catchment with the upper and middle course of the Thames flowing through agricultural land that use the water resources of the Thames to irrigate their fields. The region has also been the site of extensive industrialisation since the 18th century, with the sprawl of industry throughout London. With industrialisation there were many changes within the basin with losses of the natural environment that were previously situated in the area, an increase in air and water pollution, as well as changes to the permeability of the basin reducing the amount of recharge to the groundwater resources of the Thames. 

The Thames itself has been a major source of resources for those that are situated within the catchment, providing Food, Water, Habitats, tourism, Sports, Leisure as well as in modern times hydro-electric energy, as such there has been a dependence on the river itself for the growth that has been seen within the catchment over the past 300 years.

Pollution 

Pollution is a key issue for the sustained health of the River Thames with many sources being found throughout the basin, the pollution of the Thames has many sources from agriculture along the upper and middle course, industry within London for hundreds of years, transportation along the river and the discharge of wastewater. As such, there is a large amount of both diffuse and point sources of pollution along the course.

Agricultural activity is a major diffuse source of pollution within the River Thames basin, this is primarily found in the upper and middle course of the river and is the primary source of pollution along the river Thame, a tributary of the Thames. As a result of the misuse of products such as fertilisers and pesticides as well as poor practices for preventing the flow of these materials into the river itself, there can be a key issue for the environmental health of the river. An abundance of nitrates, phosphates and pesticides within the channel can lead to major negative impacts to biodiversity within the river with the potential for eutrophication.

The discharge of wastewater into the Thames has been an issue for the health of those in the catchment for hundreds of years with the earliest noted negative impacts occurring from 1830-1860 where tens of thousands of people died as a result of cholera stemming from the discharge of untreated sewage. Treatment methods have drastically improved since then, however, with the invention of modern treatment techniques to prevent occurrences like this. The discharge of treated wastewater into the Thames still occurs with the potential to negatively impact the health of the river if the treated water does not reach the standards outlined for them.

A major issue for the environmental health of the Thames comes from a much different source than those that have been seen before with the discharge of substances into the river, this source is plastics that enter the Thames through littering. These materials breakdown further and are found within the river as Microplastics, these plastics severely impact the environmental health of the river and the biota that lives within the Thames with the potential for bioaccumulation of these microplastics within the tissues of living organisms. It has been noted that the Thames gas some of the highest record levels of microplastics of any river globally, with an estimated 94,000 microplastics per second flow as some sites along its course. This issue of pollution is not easily managed as the diffuse pollution source can originate from a multitude of places including packaging, plastic bottles, gloves and masks to name a few, as such in order to achieve a reduction in this form of pollution it would take fundamental change on an industrial level for businesses to move away from the use of plastics. Some efforts have been made on a governmental level to reduce this form of pollution with the ban of single-use plastics such as plastic straws, however, much more is required to reduce the impact of plastics of the natural environment.

Climate Change

Climate change poses a major threat to areas within the Thames basin, with London itself extremely susceptible to flooding. The increase in the frequency and intensity of storm events within the basin as well as increases to Sea-level itself pose a major threat to the long-term stability of London going into the future. In order to reduce the threat that is posed by climate change, hard engineering strategies such as the Thames Barrier have been employed to manually regulate the water level within the Thames to prevent flooding from both the overflow of the banks but also reducing the risk of Storm surges travelling along the course of the Thames from the North Sea. However, the hard engineering solution of the Thames barrier can only function for a finite period of time with the original design of the barrier accounting for its use up to 2030, while the barrier has now been deemed sufficient protection until the 2060s. As such, there is a large air of uncertainty that hangs over the Thames and how climate change will impact the area from not only an environmental standpoint but also the societal and economic implications associated with climate change.