Author Topic: Geology Paper, part II  (Read 224 times)

Offline porkfrog

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Geology Paper, part II
« on: December 03, 2006, 02:54:16 PM »
The following is part II of III for my final Geology 100 paper. It's on Evolution. I had to answer 3 questions in 2 paragraphs. The questions were roughly.

1. Describe the main types of life during the 4 geologic eras and show an understanding of the Geologic timeline.

2. Describe what causes and what can destroy fossils.

3. Describe some theories on mass extinctions, like the one that killed the dinosaurs.


Paper to be graded on accuracy, grammar, and original thought.





“Oh, Evolve Already.” Someone I once knew had that saying for a bumper sticker. In the interest of not looking stupid, I never asked what it meant, and at the time didn’t really understand it. As the years passed I finally understood, and to this day I have yet to encounter a single phrase that said so much by saying so little. We think it all began about 4.5 billion years ago, an almost incomprehensible amount of time, with the first single cell life forms arriving about 1 billion years later. This period is known as the Precambrian Era. Geologic time is categorized into 4 Eons, 4 Eras, 12 Periods, and 7 Epochs. Most persons are more familiar with Periods, like the Jurassic, which occurred during the Mesozoic Era and is popularized as the time of the dinosaurs. Prior to the Mesozoic Era was the Paleozoic Era, a time when the first fish and reptiles appeared. We are now living in what is known as the Cenozoic Era, which began around 65 million years ago with the appearance of mammals, and is the youngest of all Eras thus far.  The most current breakdown in geologic time looks like this: Phanerozoic Eon>Cenozoic Era>Quaternary Period>Holocene Epoch.

Eventually all living things cease to live. For a fossilized record of that life to be preserved, certain things need to happen. Firstly, the deposition needs to occur in a sedimentary environment. Secondly, those remains need not be disturbed. Unless circumstances provided an absolutely ideal environment for the preservation of the organism, finding a complete fossil is rare because predators/scavengers and a host of other variables tended to scatter whatever remains that were left exposed. Geologic activity also has a huge impact on whether a fossil will “survive”. Things like compressive stress, volcanic activity, and earthquakes could destroy an existing fossil or alter the existing conditions and prevent the fossilization process from occurring. Fossils have taught us much about Earths’ history, like the age of particular rocks and also the types of organisms that preceded us in history. Before the discovery of fossilized dinosaurs, they weren’t even known to have existed. It is believed that that the myth of dragons came about from ancient civilizations having seen dinosaur fossils or their footprints. We know for a fact that dinosaurs are no myth and that they inhabited this planet for a couple hundred million years. What we don’t know for sure however, is how the entire species suddenly vanished about 65 million years ago. My research indicates that they had become a slovenly, decadent society with no real direction or central leadership, living a   gluttonous free-for-all existence. Then one day a Stegosaur named Jim “Spike” Jones said he had found the meaning of life and would lead them all to a thing he called salvation. “It’s right here in this liquid mixture I have named “Kool-Aid”, and if you drink aplenty from this cup, it shall set you free.” The rest is ancient history. Then again, there are those who think an asteroid, or a polar reversal of our magnetic poles was the causative factor. I’ll leave that for you the reader to decide.
« Last Edit: December 03, 2006, 04:43:05 PM by porkfrog »
-JoLLY
Pigs On The Wing

Offline Donzo

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Re: Geology Paper, part II
« Reply #1 on: December 03, 2006, 04:08:32 PM »
Quote
Originally posted by porkfrog
The following is part II of III for my final Geology 100 paper. It's on Evolution. I had to answer 3 questions in 2 paragraphs. The questions were roughly.

1. Describe the main types of life during the 4 geologic eras and show an understanding of the Geologic timeline.

2. Describe what causes and what can destroy fossils.

3. Describe some theories on mass distinctions, like the one that killed the dinosaurs.


Paper to be graded on accuracy, grammar, and original thought.





“Oh, Evolve Already.” Someone I once knew had that saying for a bumper sticker. In the interest of not looking stupid, I never asked what it meant, and at the time didn’t really understand it. As the years passed I finally understood, and to this day I have yet to encounter a single phrase that said so much by saying so little. We think it all began about 4.5 billion years ago, an almost incomprehensible amount of time, with the first single cell life forms arriving about 1 billion years later. This period is known as the Precambrian Era. Geologic time is categorized into 4 Eons, 4 Eras, 12 Periods, and 7 Epochs. Most persons are more familiar with Periods, like the Jurassic, which occurred during the Mesozoic Era and is popularized as the time of the dinosaurs. Prior to the Mesozoic Era was the Paleozoic Era, a time when the first fish and reptiles appeared. We are now living in what is known as the Cenozoic Era, which began around 65 million years ago with the appearance of mammals, and is the youngest of all Eras thus far.  The most current breakdown in geologic time looks like this: Phanerozoic Eon>Cenozoic Era>Quaternary Period>Holocene Epoch.

Eventually all living things cease to live. For a fossilized record of that life to be preserved, certain things need to happen. Firstly, the deposition needs to occur in a sedimentary environment. Secondly, those remains need not be disturbed. Unless circumstances provided an absolutely ideal environment for the preservation of the organism, finding a complete fossil is rare because predators/scavengers and a host of other variables tended to scatter whatever remains that were left exposed. Geologic activity also has a huge impact on whether a fossil will “survive”. Things like compressive stress, volcanic activity, and earthquakes could destroy an existing fossil or alter the existing conditions and prevent the fossilization process from occurring. Fossils have taught us much about Earths’ history, like the age of particular rocks and also the types of organisms that preceded us in history. Before the discovery of fossilized dinosaurs, they weren’t even known to have existed. It is believed that that the myth of dragons came about from ancient civilizations having seen dinosaur fossils or their footprints. We know for a fact that dinosaurs are no myth and that they inhabited this planet for a couple hundred million years. What we don’t know for sure however, is how the entire species suddenly vanished about 65 million years ago. My research indicates that they had become a slovenly, decadent society with no real direction or central leadership, living a   gluttonous free-for-all existence. Then one day a Stegosaur named Jim “Spike” Jones said he had found the meaning of life and would lead them all to a thing he called salvation. “It’s right here in this liquid mixture I have named “Kool-Aid”, and if you drink aplenty from this cup, it shall set you free.” The rest is ancient history. Then again, there are those who think an asteroid, or a polar reversal of our magnetic poles was the causative factor. I’ll leave that for you the reader to decide.


Should "distinctions" in question three be "extinctions"?  

Why the attempt at humor in your intro to attempt to satisfy #3?

Offline Golfer

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Geology Paper, part II
« Reply #2 on: December 03, 2006, 04:34:19 PM »
I'm convinced he's posting in code.  He's included all the bold items you'd find in your textbook, a few highlighted and even some underlined keywords.  Somewhere in there is a secret message describing the end of the world but I just can't crack the code.

Offline Vudak

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Geology Paper, part II
« Reply #3 on: December 03, 2006, 04:42:14 PM »
My professors would not go for your ending.  You know your's better, though.

Other than that, an interesting little paper :)
Vudak
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Offline porkfrog

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Geology Paper, part II
« Reply #4 on: December 03, 2006, 04:42:25 PM »
yes, it should have said extinctions. sorry bout that. none of that is included in my paper though. just the 2 paragraphs below all that other stuff.

ill edit the post =)


thanks
-JoLLY
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Offline porkfrog

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Geology Paper, part II
« Reply #5 on: December 03, 2006, 04:48:54 PM »
I actually don't know my professor either. It's an online course being offered thru a local community college here in the L.A. area.

I had to go for it. She said a straight scientific approach taht answered the questions was worth 45 points. One with original thought could score a max of 50. So i went for broke.

I thought it was a funny ending to a potential dry subject, depending on the audience. Then again, always be wary of the man who laughs at his own jokes harder than others laugh at them.

Besides that, do you think I answered the questions ok?
-JoLLY
Pigs On The Wing

Offline porkfrog

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Geology Paper, part II
« Reply #6 on: December 03, 2006, 05:06:38 PM »
last part. about the sea floor.  



Of all the viewing lessons, "The Sea Floor" was the most fascinating for me. I am a Marine Science Technician in the U.S. Coast Guard, but very little of what I do actually pertains to science. The oceans are considered by many, outside of Space itself, as the last frontier; a great unfathomable beast, 238857 miles closer than the Moon, but nearly as alien. We have learned more about Earths' oceans in the past 50 years than in the preceding 500 years, with vast areas of it still truly unexplored. The majority of the exploration that has been conducted has been done from the surface. Technologies including Sonar, Echo depth sounders, Magnetometers, and Seismic profilers are all employed to survey the sea floor. Submersibles are also used but account for only a small fraction of the total research. However, they enable a first hand look at the sea floor itself, the retrieval of specific samples, and high quality photographs.

   Combining the known makeup of continental crust with our newfound knowledge of the sea floor has greatly advanced the concept of Plate Tectonics. Oceanic crust being lighter and less dense than continental crust will sub-duct along zones where the two come together. Core sample studies from the sea floor show no rocks or sediments older than 200 million years, whereas samples from the continents have been aged at 3-4 billion years old. Due to magma being released along the mid-oceanic ridge, new rock is constantly being generated and accounts for the young geologic age of the sea floor. Also along the ridge itself, life is seen to exist in environments never before thought possible. An area of particular interest known as “Hydrothermal Vents”, teem with life in the form of giant worms, clams, and crabs. These vents are also the source of substantial new ore deposits, seen at the site of “black smokers”, where hydrothermal solutions rich with metallic sulfide minerals are deposited on the sea floor. Precious metals, once believed to be a non-renewable resource, are now being seen at “birth”. I am a recreational prospector/rock-hound and an old timer once said to me, “What gold we have in the Earth, is all there will ever be.” I took this as gospel because, well, I didn’t know any better. Now I could say, “Well good Sir, that’s not completely accurate. Based on…”
He has since gone to the great goldfields in the sky but I am still kneeling in the creek, albeit a little more educated, but still in the creek nonetheless.
-JoLLY
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Offline porkfrog

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Geology Paper, part II
« Reply #7 on: December 05, 2006, 11:57:03 AM »
I rcvd an A on 2 of the 3 papers I turned in. The 3rd still hasn't been graded. Thanks for all the input/advice/proof reads that you all contributed.
-JoLLY
Pigs On The Wing