lesson created by janey cohen for the santa barbara museum

11
In Puja and Piety, stone is one of the most universal ma- terials used to make sculptures, shrines, and votives. It is part of Hindu belief that if a stone is shaped into a func- tional object, it becomes filled with a sacred essence and is used as part of puja (worship). Even stone un- changed by human hands can be held as sacred. In thousands of temples throughout India, svayambhu, a natural, uncarved stone, is the primary murti, or embodiment of the Divine. For over 2500 years, sculptors have been using stone as their medium. By knowing which stone would work best for their purposes, early artisans were able to create these enduring works of religious art. Lesson created by Janey Cohen for the Santa Barbara Museum of Art ROCK ON! Temple Sculpture with Dancing Ganesha. The popular God of Auspiciousness, distinguished by his elephant head. India, Uttar Pradesh, 11th century. Sandstone. Lent by Anonymous in Memory of Ann Witter.

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Page 1: Lesson created by Janey Cohen for the Santa Barbara Museum

In Puja and Piety, stone is one of the most universal ma-

terials used to make sculptures, shrines, and votives. It is

part of Hindu belief that if a stone is shaped into a func-

tional object, it becomes filled with a sacred essence

and is used as part of puja (worship). Even stone un-

changed by human hands can be held as sacred. In

thousands of temples throughout India, svayambhu, a

natural, uncarved stone, is the primary murti, or

embodiment of the Divine. For over 2500 years,

sculptors have been using stone as their medium. By

knowing which stone would work best for their

purposes, early artisans were able to create these

enduring works of religious art.

Lesson created by Janey Cohen

for the Santa Barbara Museum of Art

ROCK ON!

Temple Sculpture with Dancing Ganesha. The popular God of Auspiciousness, distinguished by his elephant head. India, Uttar Pradesh, 11th century.

Sandstone. Lent by Anonymous in Memory of Ann Witter.

Page 2: Lesson created by Janey Cohen for the Santa Barbara Museum

Did you know that every

mineral has a set of

characteristics that is unique

to that mineral alone and

can be used to identify it? By

learning to test for traits such

as hardness and luster,

streak and density, you can

be a geologist right in your

own backyard.

Head of Shiva. India, Uttar Pradesh, Mathura, 6th century. Mottled red sandstone. Santa Barbara Museum of Art, Gift of Pratapaditya and Chitra Pal, 2008.47.5

Page 3: Lesson created by Janey Cohen for the Santa Barbara Museum

Collect several “mystery” minerals.

Try finding different rocks from

your yard or from a rock collector.

Choose minerals that have not

gone through a rock tumbler.

Give each of your minerals a

number. Use this chart

to keep track of the

characteristics of your minerals.

Mineral # Luster Hardness Streak Density

(g/ml)

Page 4: Lesson created by Janey Cohen for the Santa Barbara Museum

You will need:

Several samples of unknown minerals

Magnifying glass

Penny

Lamp

Steel nail

White bathroom tile

Glass plate

Kitchen scale that uses grams

Water

Graduated cylinder

Rock On!

Detail of Temple Sculpture Representing Enshrined Bodhisatva Manjushri Seated on a Lotus, Uttar Pradesh, 11th century. Cat. 165.

Page 5: Lesson created by Janey Cohen for the Santa Barbara Museum

Luster Test– The appearance of certain

minerals changes when you shine a light on

them. This reflected light is called luster. Use

the light and the magnifying glass and look

at the surface of your mystery mineral. Use

words such as dull, metallic, glassy, or sparkly

to describe the luster.

Streak Test- Take the piece of white tile and

put it on a flat surface. Push the mineral

down onto the surface and rub it across.

Does it make a streak? Write down the color

of the streak.

Page 6: Lesson created by Janey Cohen for the Santa Barbara Museum

Hardness Test- First, use your fingernail to

see if you can scratch your mineral. If you

can, it is less than 2.5 on the hardness

scale.

Try to scratch the mineral with the penny.

Does it make a mark on the rock? If so, the

mineral is under 3.5 on the hardness scale.

Try scratching it with the nail. If it gets

scratched, it’s under 5.5 on the scale.

Finally, if your mineral didn’t get scratched

by any of the first three items, use the

mineral itself and see if it will scratch the

glass. Put the glass on a flat surface and

use the rock to scratch the glass. If it does,

it’s over 6 on the hardness scale.

Page 7: Lesson created by Janey Cohen for the Santa Barbara Museum

Density Test- Finally, you’ll test the density of

your minerals. First, find the mass of your rock

with a scale in grams and write it down.

Next, fill a graduated cylinder half full of

water. Note the level of water in milliliters.

Carefully place the rock in the water. Note

the new higher level of water that the rock

has displaced.

Calculate how many milliliters of water the

rock displaced. Divide the mineral’s mass in

grams by the volume of water in milliliters to

get the density of each mineral.

Page 8: Lesson created by Janey Cohen for the Santa Barbara Museum

Solving the Mystery– Compare your results to

these common minerals and see if you

might have any close matches. If your results

don’t match these, try doing an Internet

search using the words

“properties of minerals”. properties of minerals

Mineral Luster Hardness Streak Density (g/ml)

Graphite Metallic 1 Black 2.1-2.3

Halite Glassy 2.5 No color 2.2

Calcite Glassy 3 No color 2.7

Magnetite Dull 5.5-6.5 Black 5.2

Pyrite Metallic 6-6.5 Gold 4.9-5.2

Feldspar Glassy 6-6.5 Different Colors 2.5-2.75

Quartz Glassy 7 Different Colors 2.6-2.7

Sandstone Dull 6 Light colored 2.2-2.8

Page 9: Lesson created by Janey Cohen for the Santa Barbara Museum

Why do rocks and minerals have different

characteristics? They’re made out of different

elements that are put together in different

crystal structures.

You may have chosen quartz in your

experiment. This common mineral is made from

silicon dioxide (silicon and oxygen).

A diamond is made out of pure carbon. So is

graphite. The difference is that their crystals are

not organized in the same way. It’s like taking

an equal number of blocks and arranging them

in different ways. They make different structures,

but they’re still the same blocks.

A gander from Nagarjunakonda stupa. Andhra Pradesh. 2nd century.

Page 10: Lesson created by Janey Cohen for the Santa Barbara Museum

A sculptor needs to take into

account all of the characteristics of

a stone before beginning to work

with it.

Stone comes in many lusters and colors, and this will affect

the overall beauty of the piece. In ancient times, before

transportation made it easy to move stone around, the

density of the stone was also a very important factor in

choosing stone. Centuries ago, sculptors simply needed to

use the rock that was natural to their locale.

The hardness is the

most important

characteristic.

Ease of carving is

important, and

softer rock is easier

to sculpt, but it

needs to be hard

enough not to

break and to hold

up over time.

Page 11: Lesson created by Janey Cohen for the Santa Barbara Museum

This presentation was created by SBMA for instructional use only

and is not to be altered in any way, or reproduced without at-

tribution

Lesson created by Janey Cohen, Santa Ynez Valley High

School, for the Santa Barbara Museum of Art

For further information about these or other Education and

Outreach Programs, contact Rachael Krieps at

[email protected]

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