A presentation for students that looks at the types of weat - PowerPoint Presentation

Slide1

A presentation for students that looks at the types of weathering, rusting and rotting that can be found in our cemeteries

Wearing Down: Weathering,

Rusting

& rottingSlide2

The breaking down of rock is called weathering.

What is Weathering?

There are two types of weathering.

Chemical

weathering

Most weathering is the result of both kinds.

Physical

weathering

Different rocks weather at different rates depending on how hard they are. How hard they are depends on what they are made of.Slide3

Chemical weathering is the chemical breaking down of rocks.

There are many different minerals in rocks. When water and air react with these minerals the new minerals formed are usually softer and the rock begins to crumble.

Chemical Weathering

When chemical weathering happens, a new substance is made.Slide4

Limestone and Marble

Limestone and marble are made of calcium carbonate. A special type of weathering occurs with limestone and marble.

Carbon dioxide in the air reacts with rainwater to form carbonic acid

Carbon Dioxide + water carbonic acid.

Limestone and marble react with acid so when this acidic water seeps into cracks and fissures it can dissolve quite large amounts eventually turning into caves and archways.

Chemical Weathering Slide5

Limestone Weathering

Lime

stone is a soft

sedimentary rock, prone to chemical weathering.

Example 2 shows weathering on the carved edges of one side of the inscription plaque.

Example 1 shows

delamination

on the surface of the stone. The surface is lifting and flaking around the inscription.

2

1

Chemical Weathering Slide6

Examples of Limestone Weathering

Images show a combination of chemical and physical weathering on this memorial in Dunedin’s Southern Cemetery.

The northern face of this monument may have been worn away with water turning the calcium carbonate into carbonic acid.

It is now a warm roosting site for sparrows who are contributing to the wear.

Chemical Weathering Slide7

Examples of Marble Weathering

Slowly over time the calcium carbonate reacts with carbon dioxide in the air or in rainwater to form carbonic acid.

The acid wears away the marble from around the inserted lead letters gradually leaving them slightly proud of the surface stone.

More and more water gradually wears the marble away around the lead pegs and the letters gradually come loose.

Chemical Weathering Slide8

Experiment:

Can you work out what factors affect

how quickly

some rocks

are attacked by acid?

How

will you measure the rate of reaction?

How will you make it a reliable test?

How will you make sure your tests are safe?

How will you record your results?

What equipment will you need?Limestone chips /or marble chips (size of chips might be a factor to investigate?)

Dilute hydrochloric acid

Bunsen burner, tripod, gauze & heatproof matThermometer

Balance or digital scalesTimer

Flask with stopper and delivery tubeBasin and Measuring cylinders

Temperature of acid (

0

C)

Time to collect gas

Concentration of acid (M)

Time to collect gas

Choose a factor to investigate. This might be temperature or perhaps how strong the acid is. Are there other factors to consider? Slide9

Granite

Granite is formed by the solidification of magma underground. It is called an igneous rock.

Granite often contains cracks and joints.

Water seeps into the cracks and some of the minerals in the granite gradually turn to clay causing the granite to crumble.

Chemical Weathering

This is a very slow process and there is little evidence that headstones made from granite are starting to weather chemically.Slide10

When the physical weathering of rocks happens no new substances are made.

Rocks instead are broken into smaller and smaller pieces in a variety of ways that include temperature changes, freezing and thawing and plants.

Physical

weatheringSlide11

Repeated heating and cooling of rocks can cause cracks to form.

During the day the part of the stone facing the sun heats up more quickly than the side facing the shade, and expands. At night the sunny side of the stone cools and contracts. The continual expansion and contraction eventually causes cracks in the rock.

This kind of weathering is sometimes called onion skin weathering or exfoliation and can also be a cause of the

delamination

seen in slide 5 on the limestone headstone.

Heating and cooling

Physical Weathering Slide12

Water gets into cracks in rocks. When water freezes it forms ice.

When water begins to freeze it expands. Water between 4

o

C and 0

o

C expands. A lump of ice has a greater volume than the liquid water that it was made from.

Freezing causes expansion of cracks and splitting or

spalling

of headstones which can cause even greater damage in future freezing and thawing.

Freezing and Thawing

Physical Weathering Slide13

Experiment:

What equipment will you need?

Small plastic or glass bottle with tight fitting lid

Water

Freezer

Ice cream container with fitting lid.

What happens to water when it freezes?

Try this experiment at home.

Fill the bottle with water right to the top. Screw on the lid tightly. Place the filled bottle in the ice-cream container and fit the lid.

Place in the freezer over night.

Describe how the bottle and water look next morning.

Physical Weathering Slide14

As the cracks open up water enters and undermines the stone especially in freeze thaw situations

.

Temperature Changes

The base of this sandstone memorial is beginning to fracture and flake on the sunny side of the

memorial

. Cracks are running

parallel

and at right angles to the

surface.

Physical Weathering Slide15

Plants cause physical weathering.

Some of the seeds may fall, be blown, or dropped by birds into cracks in rocks and develop into seedlings.

As the tree grows, the roots act like a crowbar wedging rocks apart.

Plants

Physical Weathering Slide16

Windblown or bird dropped seeds often grow unnoticed in cracks and can remain safe from

weedkillers

.

When the trees become larger the roots can undermine the headstone foundations, and trunks can push and displace the headstone, or even subsume it completely.

Physical Weathering

Wilding Tree DamageSlide17

Physical Weathering

Left:

Foetid

iris and holly growing in cracks between and behind headstones.

Above: Agapanthus is a major nuisance at an Auckland cemetery.

Lower left: Ivy clings by growing into the surface of softer stones and can never be completely cleaned.

WeedsSlide18

A wide variety of mosses, lichen and fungi can be found growing over cemetery headstones.

Mosses, Lichens and Fungi

Although lichens are usually the first living organisms to

colonise

rocks the process of wearing down the stone is very slow and they do less actual damage to the stone than some cleaning processes.

Physical Weathering

A species of encrusting lichen called

Xanthoria

ligulata

commonly found on coastal rocks.Slide19

Mosses can be found

colonising a range of different stone types especially in areas where water accumulates or pools.

Limestone is a porous rock that retains water. Limestone headstones that are lying with their backs in contact with the ground are often covered in a thick layer of moss in damper areas.

Physical Weathering

MossesSlide20

fungi & Lichen staining

Red or black staining on white marble detracts from the look of the headstone .

The red

discolouration

is caused by

lichen staining which emanates from the microscopic growths which inhabit the spaces behind the lead letters.

The black

discolouration

is caused by a fungus which grows on the surface of the marble.

Physical Weathering Slide21

Various lichens including the very common

Xanthoparmelia

tasmanica grow over the surfaces of headstones making them difficult to read inscriptions.

Lichen: Surface Encrustations

Xanthoparmelia

tasmanica

is the botanical name for a pale green lichen that thrives in damp urban environments. It can be found growing on rocks, tree trunks and roof tiles, as well as on asphalt and is a common lichen found in our cemeteries.

Physical Weathering Slide22

Another is uneven soil compaction. After a burial soil was used to refill the hole but this was not compacted. Over time this un-compacted soil settles and creates

sinkage

.

Movement of soil

The stones in the cemetery are also open to other types of wear and tear. One of the most common is the gradual movement of soil down a steep slope. Sometimes the headstone and the corner posts will all shift to the same degree.

Physical Weathering Slide23

Some older cemeteries were not developed with adequate field drains. Some of the soil creep and compaction problems can be due to a lack of, or poor drainage arrangements.

Poor Drainage

In many places cemetery headstones are affected by being located in low lying swampy places.

Physical Weathering Slide24

Whole or parts of memorials can be smashed.

Vandalism

Deliberate vandalism is a problem in many cemeteries. Examples from left include…

Physical Weathering

Graffiti painted or incised on headstones

Marble decorations deliberately chipped off

Stelae

pushed overSlide25

Examples of a range of chemical and physical weathering of rocks can be found in almost all of our cemeteries. The natural processes of wearing away and breaking down of cemetery materials is occurring all the time.

Maintenance of Cemeteries

Maintenance and conservation of our cemeteries is an important and ongoing task if the historic cemetery is to remain for future generations. For homework visit

http://www.cemeteries.org.nz/

and click on the left hand link to “Cemetery Conservation.” Assign problems from the slide show or have groups or individual students choose to investigate and find a possible solution from the site. Revisit each of the slides and encourage the class to discuss solutions to some of the problems in this slide show.

Discussion: What are the solutions to some of these problems?