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Weathering: The Response of Rocks to a New Environment By A. Orgonik

Weathering: The Response of Rocks to a New Environment By A. Orgonik

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Page 1: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Weathering: The Response of Rocks to a New Environment

By A. Orgonik

Page 2: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Caumsett State Park

How is this rock’s environment different from where it formed?

Page 3: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Boulders in the woods at Caumsett.

Page 4: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Let’s take a closer look at these rocks. What beautiful cranberry mineral is in this one?

Page 5: Weathering: The Response of Rocks to a New Environment By A. Orgonik

What weathering processes might be going on in these rocks knowing (and seeing here!) the climate of Long Island?

Page 6: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Water in what state?

What is happening here?

Page 7: Weathering: The Response of Rocks to a New Environment By A. Orgonik

What weathering process appears to be happening here?

Is it a physical or chemical process?

Page 8: Weathering: The Response of Rocks to a New Environment By A. Orgonik

What weathering process is happening here?

Page 9: Weathering: The Response of Rocks to a New Environment By A. Orgonik

A close-up view!Is this chemical or physical?What weathering

process is happening here? EXFOLIATION

PHYSICAL

Page 10: Weathering: The Response of Rocks to a New Environment By A. Orgonik

MONTAUK POINT: Long Island, NY

Page 11: Weathering: The Response of Rocks to a New Environment By A. Orgonik

What mineral is the cause of this beautiful purple/red sand?

Page 12: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Remember this one?

Page 13: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Where does sand come from? What processes formed the sand we see here?

Page 14: Weathering: The Response of Rocks to a New Environment By A. Orgonik
Page 15: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Sand is the remains of weathered and eroded rock!

Page 16: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Welcome to Huntington Cemetery! Step inside to another real-life weathering laboratory!

Page 17: Weathering: The Response of Rocks to a New Environment By A. Orgonik
Page 18: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Wow! We haven’t even stepped inside and we have evidence of weathering in the gate!

What process is this and is it physical or chemical?

Page 19: Weathering: The Response of Rocks to a New Environment By A. Orgonik

We are going to look at cemetery rocks…(tombstones!) and observe the weathering that has occurred in them.

Page 20: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Since tombstones are dated we can even determine how long the weathering has occurred!

Page 21: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Here is a typical marble tombstone which used to be a very popular rock for cemeteries.

What mineral largely composes the rock marble?

What is the hardness of this mineral? Why was it a good rock for tombstones?

Page 22: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Here is another type of tombstone. It is made up of slate.

Page 23: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Compare the two tombstones in the next picture. How do they differ in terms of the types of weathering that has occurred to each?How do they compare in appearance? Which appears more weathered?

Page 24: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Marble Slate

Page 25: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Marble Slate

Which tombstone is older?

Page 26: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Marble Slate

This means that rocks can weather at different rates!

Page 27: Weathering: The Response of Rocks to a New Environment By A. Orgonik

This is called “Differential Weathering”

Rocks weather at different rates due to differences in mineral composition.

Some minerals are more stable at the earth’s surface than others! These take longer to weather.

Page 28: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Calcite is very unstable at the earth’s surface in certain climate types. Which type in particular?

Page 29: Weathering: The Response of Rocks to a New Environment By A. Orgonik

What weathering process causes the tombstones to “dissolve”? Is this chemical or physical?

CO2 CO2

Page 30: Weathering: The Response of Rocks to a New Environment By A. Orgonik

But even slate tombstones are not immune to weathering!

What weathering process is occurring here? Is it physical or chemical?

Page 31: Weathering: The Response of Rocks to a New Environment By A. Orgonik

More tombstones undergoing weathering! What process might be happening here, knowing the climate of Long Island?…

Page 32: Weathering: The Response of Rocks to a New Environment By A. Orgonik
Page 33: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Another tombstone weathering (for almost 200 years!)Its distinct color indicates one weathering process going on! Which one?

Page 34: Weathering: The Response of Rocks to a New Environment By A. Orgonik

What other process is occurring?

EXFOLIATION

Page 35: Weathering: The Response of Rocks to a New Environment By A. Orgonik
Page 36: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Slatey cleavage seen due to weathering!

Page 37: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Why does the climate of Long Island contribute to exfoliation and frost action of these tombstones?

Page 38: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Living organisms can also weather rock!

Page 39: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Here are lichens, organisms that can make a living on bare rock (in this case a tombstone…)

Lichens secrete acids that dissolve rock!

Page 40: Weathering: The Response of Rocks to a New Environment By A. Orgonik

REVIEW: What types of weathering processes can you see here?

EXFOLIATION

Page 41: Weathering: The Response of Rocks to a New Environment By A. Orgonik

Another view of the previous tombstone

Page 42: Weathering: The Response of Rocks to a New Environment By A. Orgonik

The climate of L.I. (its fluctuating temperatures) is even causing these tombstones to heave up out of the ground!

Page 43: Weathering: The Response of Rocks to a New Environment By A. Orgonik

It’s time for us to leave, but weathering processes continue 24-7!

What will this place look like in another 50 years?