Geology in Essex Walls
Blocks and cobbles of building material, dug from nearby pits in the land or from seashores, have long been used in the construction of thousands of walls in the region, especially church walls. Materials used in churches and walls in and around Essex may thus broadly reflect underlying geology. These materials could therefore provide some access to geology otherwise hidden beneath the landscape.
The question is, how good a reflection is this? Is there a pattern to wall building that reflects the underlying geology in any meaningful way? Does the pattern also reflect a configuration of transportation of materials from the coast and from outside the area? This project should enable us to test whether there are any such patterns.
Church and tower walls, garden and cottage walls (with permission) and estate walls all provide evidence.
Practical method for cobble wall observations:
‘Cobbles’ are rounded stones between pebble size and boulder size. It is not necessary to note any sizes for this study, apart from exceptional occurrences. ‘Blocks’ are not rounded and were shaped by masons or otherwise roughly broken by builders. We do know of broken cobbles and rounded blocks but let us not get tied up with definitions. The term ‘material’ includes both stone and artificial products. Cobbles can be split or ‘knapped’.
Take a camera, note pad and pencil.
It is impractical to complete a rapid statistical record for each wall. Our procedure, although subjective, is a simple and practical ‘frequency of use’ recording for each type of material.
This exercise aims at characterising walls that are built with cobbles, with or without random blocks and bricks. It is not aimed at characterising wholly stone-built churches and walls, such as Cotswold limestone or Kentish Rag constructions, or for brick buildings and walls with decorative stone details.
IMPORTANT 1: During observation, in assigning materials to their frequency categories, take the whole of any church or other construction as one item; i.e. do not attempt to separate different parts of a church, different ages of construction or different sections of repair or reconstruction. Consider the whole, including any recent extensions and assign the occurrence grades to the set of buildings as a whole. Sometimes a quick (20-minute) walk around a church enables a reasonable overall judgment.
IMPORTANT 2: do not worry about how far upwards (or downwards) you can see; just give an impression from what you can comfortably observe.
Use these approximate Frequency Categories:
Abundant (A), (A*) – the material makes an immediate visual impact and often represents a significant proportion of the construction. Add a star if the material appears to represent more than about 90% of the whole.
Common (C) – the material is present in significant numbers so as to be easily recognized - i.e. between about 50 and up to around 50% of the total church or wall.
Occurs (O) – around 10 to 50 pieces seen. No need to be exact.
Rare (R) – typically less than 10 examples of a material, often only one or two pieces.
Materials seen in local churches and walls include:
Flint is extremely variable in size, colour, texture and shape. By far the best way to ‘get your eye in’ is to view as many different verified flints as possible. Flints that have been quarried from Chalk are very often black inside with a white surface; they may be either whole or broken. Some flints were carefully broken or ‘knapped’. Skilled knapping produced beautifully shaped blocks, squares and special shapes in flint for some walls. Many flints from gravel and glacial till deposits are stained brown to red internally with iron minerals. Some are brown, grey or black on the outside or quite mottled. Many are in strange shapes; some have holes in or through them. Many such flints are broken, showing characteristic conchoidal fracture surfaces. Red and pink flints, usually very crackled, have been heated in fires. Flint pebbles and cobbles were rounded on ancient seashores and incorporated into gravel deposits. If possible, note the proportions of flints used as cobbles (naturally-worn), ‘raw’ nodules (unworn, as they came from the Chalk), or ‘knapped’ (split or shaped artificially. Flint frequently forms the largest proportion of a cobble wall.
White, occasionally mottled with pink or greenish minerals. Not sugary, but crystalline in texture. Often with small cavities that show a ’twinkle’ of tiny quartz crystals. Tough, sometimes ‘knobbly’, occasionally quite well rounded. Sometimes bright, pure white.
Not usually as smooth looking as quartzite. Vein quartz often looks slightly translucent.
NOTE: if both quartzite and vein quartz appear in the same frequency category, assess which is the more abundant in one church or wall, as this might be geologically relevant.
Two categories may usefully be distinguished in Essex walls:
‘Bunter’ quartzite and other quartzites.
The ‘Bunter’ stones are usually very smooth cobbles of fine-grained or sugary sandstone. Colour varies from white through pink to brown, often mottled. Other types of quartzite are dark brown or coarser in texture, usually these all look ‘sugary’ when seen close-up. Count these all simply as ‘quartzite’. ‘Bunter’ cobbles are commonly seen to have split along flat planes. Mostly they are less than about 6” or 15cm across. Opaque looking c.f. vein quartz.
These are pale quartzites that are extremely tough. They are often larger than 6” or 15cm across, and are sometimes very large. They are normally not rounded or wholly smooth; sometimes they look gnarled. They have a very fine ‘caster sugar’ texture. White to pale creamy brown in colour unless weathered and stained grey to dark brown.
Aka ‘Hertfordshire Puddingstone’, although much is found in Essex. Make sure you can distinguish this stone from ferricrete (described below). This extremely tough stone is the conglomerate equivalent of sarsen. It consists of rounded to broken flint pebbles set in a pale quartzite matrix. The flint pebbles are usually (but not always) brown or reddish with a black ‘rind’. Characteristically the cobbles of puddingstone have split straight across both matrix and pebbles, due to their equal degrees of toughness, providing a flattish plum pudding picture. Some surfaces may be shiny. Sometimes shards of flint are seen in matrix.
A brown to black conglomerate of flint pebbles and fragments set in a ‘rusty’ sandstone. The sand is much less tough than the flint, so the cobbles do not show breaks equally across flint and sandstone. Instead, the pebbles protrude like plums in brown cake. Flint pebbles may be whole or broken. Old ferricrete may look almost black and may contain cavities from which flints have dropped out. Ferricrete with no pebbles looks like quartzite or dark red, brown or blackish sandstone - these can be counted as ferricrete here. (But see clinker below - note that ferricrete has a sandy matrix between flints, unlike most clinker.)
Usually in rounded lumps but occasionally in rectangular blocks. Pale grey when fresh, it turns to brownish or buff quite rapidly. Frequently weathered buff or deep yellow with a spalled onion skin texture. Very often cementstones are deeply weathered and their powdery-looking spalled surfaces are either ‘dished’ outwards or inwards within the wall surface. Very occasionally round borings are seen - holes made by marine molluscs. May have infilled cracks filled with white to brown or yellow calcite (‘septa’) which give these the name ’septarian nodules, or ’septaria’. Septa are seldom seen in walls, however.
Blocks of various kinds of limestone were commonly re-used within walls. Note these merely as ‘Limestone’ regardless of type and origin: do not attempt to categorise different limestones unless it is very obvious to you (e.g. perhaps Greensand and Purbeck). Limestone blocks exist in a variety of shapes due to former uses as quoins (cornerstones), flooring, steps, gravestones, etc. Do not assess the quantities of limestone (or sandstone) used for quoins, arches, windows, ledges and copings: these might be noted (e.g. if made of tufa, chalk), but they do not form the most essential part of this wall survey because it can be very difficult to decide the origins of these stones.
Although chalk is a limestone, it is distinctively pale and soft. Usually pure white, it can also be grey and less crumbly (‘Chalk Rock’) and difficult to distinguish from cementstone (above). However, it is usually seen as blocks, maybe with right-angled corners, whereas cementstone was rarely ‘shaped’ and is frequently seen as rounded ‘lumps’. Both chalk and cementstone tend to weather ‘inwards’ but chalk usually remains white or grey.
Off-white stone with an ‘open’, spongy or cellular textured limestone. It is very local in occurrence, as it forms in limy deposits around plant fragments in rivers. Cut into blocks or used in lumps. Some compact varieties of tufa used in buildings are called travertine.
Very tough, smooth pebbles, usually less than 4” or 10cm in size. They are often black-and-white, either black rock veined with white quartz or a ‘breccia’ of white or pale rock fragments set in a black matrix (ground mass). See pictures for distinctive textures. We use the term ‘Cornish’; however, these have been brought by rivers from anywhere in and around the area of SW England.
Brick and tile.
Although not natural materials, these are also included in the survey if they occur within the cobbled wall fabric, as these provide information on re-use of building materials. Note any Roman material, if you are able to decide.
Usually these are melted or semi-melted masses of brick from brickworks. Many garden walls were made from these, notably up to the 1930s. Very occasionally they are seen in church walls. Usually they look frothy, bubbly or semi-molten and are black to very dark brown. Occasionally a brick end may be spotted within the mass. Not to be confused with the very similar-looking ferricrete. Usually clinker does not contain flints, but this has been seen, and can be confused with ferricrete. Clinker often looks melted in parts.
Occasionally you see a glacial ‘erratic’, or a stone transported by humans, that looks ‘different’. Some erratics are Scottish or Scandinavian igneous or metamorphic rocks and a few are truly beautiful and fascinating. Best take a photo and note its exact position in the wall, and then we can go to have a look. Similarly, Thames gravels brought exotic rocks to Essex, such as volcanic ignimbrite from North Wales and conglomerate from South Wales, as well as the ‘Cornish rock’, ‘Bunter’ cobbles and vein quartz. Rare ‘other’ rocks should be noted; they add to the geological story and can be significant despite their rarity.
Images of materials will be added to this website soon.
Where to look:
For our purposes, ’Essex’ consists of the old county, pre-GLC.
There are hundreds of churches and walls in Essex to look at but we are happy if you wish to stray into adjoining counties; just stop if you find you are in Yorkshire. Don’t worry if you are duplicating the efforts of others: we shall aggregate results rather than issue wall lists to different people. To help you choose, see guidebooks, plus individual church web sites and general websites such as
People of adjoining counties:
please feel free to use this scheme and add to the map. Geology does not stop at county boundaries. Some differences would show up, e.g. Crag rocks would feature in Suffolk walls.
For images and explanations of pebbles and cobbles seen in the region, please refer to the folder Pebbles in Essex and beyond published by Essex Rock and Mineral Society. Together with the individual images, this chart will help distinguish the most frequently seen materials in Essex cobble walls.
Survey forms will be distributed to ERMS meetings
and to Broomfield U3A, EFC Green Centre at Pitsea, The Naze Tower at Walton, etc.