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Senior University Geology Field Trip

November 5, 2012 8:45 am – 4:30 pm

Georgetown’s Amazing Geology

with Don, Rocky, & Sandi

Explore , Photograph, & Sample . . . . .

world famous rocks modern perched water table modern aquifers supplying our drinking water

10, 000 years old black waxy glacial clays

135 million year old Rudist reefs

45 million year old Balcones Fault

Our Travel Schedule

8:45 to 9:00 am Briefing at The Oaks

9:10 to 9: 30 STOP 1 - Perched water table

9: 40 to 10:00

Berry Creek Pond

STOP 2 - Black Waxy clays

10:15 to 10:30

Walgreens, Williams Dr

STOP 3 - Rudist reefs

10:35 to 10:40

Lake Georgetown spillway

STOP 4 - Reef in D.B. Woods road cut

10:50 to 11:15 STOP 5 - Rudists and grasses

11:30 to 12:15

Wolf Ranch Mall

STOP 6 - Buda limestone cliff & faults

Celebration Church

12:30 to 1:30 LUNCH – French Quarter Grill

2:00 to 4:00 STOP 7 - nner Space Cavern

4:30 Return to Sun City

Definitions

Mineral: natural occurring constituent of all rocks

Limestone: sedimentary rock composed of the mineral Calcite

Shale: sedimentary rock composed of one or more Clay minerals

Sandstone: sedimentary rock composed of the mineral quartz

Ground water: rain water filling rock voids

Water table: top of the ground water

Aquifer: rock containing fresh water that can be recovered in a well

Normal fault: fracture in bed rock with measurable displacement

Stromatolites: Shallow water blue-green algae deposits

Briefing at The Oaks, Sun City

Age of the Rocks that we saw

Cretaceous Period

Eagleford Shale 120 feet

Buda Reef 60 feet

Del Rio Shale 60 feet

Georgetown Limestone 100 feet

Upper Dense limestone 30 feet

Rocks at the surface in Sun Cit y

Edwards Limestone 380 feet

Reef & Reef debris aquifer limestone 100 feet

Comanche Peak limestone 50 feet

Upper Walnut limestone 100 feet

Lower Walnut limestone 100 feet

Glen Rose Limestone 400 feet

Trinity sandstone 0 to 100feet

Ouachita Mountain complex folds and thrust faults

Trinity sandstone aquifer

0 to 100 feet

Geography when our limestones were formed about 115 million years ago

Rocks Exposed at Sun City

Berry Creek not eroded this deep

Geological Cross Section

Williamson County, Texas

Springs

Fossils you may have stumbled over

Bryozoa (sea moss) Stromatolites (Algae)

Brachiopods

(symmetrical shells)

Gastropods (snails)

Pelecypods (clams)

(asymmetrical shells)

Cephalopods & Ammonites Corals

On the road . . .

Stop 1 - Perched Water Table at Berry Creek Pond

Stop 1 - Perched Water Table

Pavilion at Berry Creek Pond

Berry Creek Pond (stock tank)

Williams Dr. Gate

Village Center

Reef

Reef water filled=a perched water table

Stop 2: Holding pond at Walgreens on Williams Dr

. . .the base of the pond is on impervious limestone!

Stop 2: Waxy Clay on weathered Georgetown Limestone

Walgreens on Williams Dr

What’s the black surface dirt?

Stop 2: Waxy Clay on weathered Georgetown Limestone

Walgreens on Williams Dr black waxy clay weathered

Georgetown limestone un-weathered

Georgetown limestone

Stop 2: Waxy Clay on weathered Georgetown Limestone

10,000 year old black waxy clays weathered & eroded from Rocky Mountains in New Mexico

Stop 3: layered limestone with rudist reefs

What rocks are these?

Lake

Georgetown

Spillway

Stop 3: layered limestone with rudist reefs

Lake Georgetown Spillway

Lake Georgetown Spillway North Rock Wall

Stromatolites cap layer

Eoradiolites Rudist Debris Bank

Stromatolite layer

Rudist Reef-forming Sea Shells

Lake Georgetown Rudists

Rudists: the exotic moundbuilding Rudist Clams that became extinct at the end of the

Cretaceous

Length: 6 inches to 3 feet!

WHAT IS A RUDIST REEF?

A clam-like colonial (successive generations build on top of each other giving the reef vertical strength that minimizes compaction of the reef when buried). The rudist sea shell is shaped and sized like an inverted old fashioned glass Coke bottle. They occur in the

Cretaceous Period 145 to 65 million years ago and are the equivalent of corals of today and other geological

Periods.

The rudist fossil is the “limestone” shell of the marine organism and it is very delicate so it often weathersout leaving a round hole.

Stromatolites: blue green algae

Stromatolites grow in shallow water

Modern Stromatolites Stromatolites preserved as rocks

Stop 3: layered limestone with rudist reefs

Stop 3: layered limestone with rudist reefs

Stop 3: layered limestone with rudist reefs

Lake Georgetown Spillway

Stop 4: Limestone Reef Outcrop

Road Cut, D.B. Woods Road

D. B. Woods Road - reef outcrop

. . . the reef ‘matrix’ resists compression from the rock layers above, maintaining its shape

Stop 5: rudist fossils in country rock, Texas grasses

Wolf Ranch Shaded Walk

Stop 6: Eagle Ford gas source rock, Buda cliff, Texas

Crushed Stone Quarry, Balcones Faults

Celebration Church Overlook

Inner Space

Cavern

Balcones Faults

Up

Down

Up Down

Celebration overlook

Inner Space

Cavern

Balcones Faults

Note:

Black Waxy

Celebration overlook

Lunch: French Quarter Grill: Round Rock

Stop 7: Inner Space Cavern Tour

Stop 7: Inner Space Cavern Tour

Balcones Fault

Flint

Dolomite

Limestone

ROCKS OF THE INNER SPACE CAVERNS

Limestone is the original rock type which when buried can have the Ca partially replaced by Mg due to the movement of fluids being expelled by compaction of the whole rock column creating dolomite.

Dolomite does not “ fizz ” in acid until you scratch it into a powder, then if “ fizzes ” . Otherwise, it look just like limestone.

Flint is silicon dioxide and is thought to be the silicon dioxide of sponge quills called spicules sort of like the quills of a porcupine, but a marine animal that shared the reef with the Rudists and other reef organisms. The thin, discontinuous flint layers are thought to be formed when a storm swept a number of individual sponges off the reef and deposited their dead bodies in a “ quiet ” place out of the way of the waves and tides. Since the spicules become plastic as the organic sponge bodies decay, the plastic layers of flint during burial and compaction are often squeezed into “ lumpy ” and discontinuous “ blobs ” ..

The end of a perfect day!!!

Self-drive Field Stop

The next 4 slides describe a self-drive field stop that you could do with family or friends. The destination is Blue Hole City Park in Georgetown.

On the drive from Wolf Ranch Shopping Center to the park, you will cross the Balcones Fault just east of Interstate 35.

At Blue Hole Park, rudist fossils in the Edwards

Limestone are visible on the rock outcrop (rock face).

Enjoy!!

Self-drive Field Stop: Blue Hole City Park

Balcones Faults & Edwards Limestone Rudist Reef

Blue Hole Park

Austin Ave

Wolf Ranch

Self-drive Field Stop @ Blue Hole Park: Balcones Fault

Blue Hole Park

Up

Down

Austin Ave

Self-drive Field Stop @ Blue Hole Park: Balcones Fault

Blue Hole Park

Up

Down

Self-drive Field Stop @ Park: Edwards Rudist Reef

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