The coal bed problem: correct!

Boudinage (with attitude of plunge for good measure)! Boudinage occurs when a rigid rock is extended and stretched to break apart its surrounding rock that is less resistant to deformation. The pieces formed are called boudins.
1. It depends on the information given. If you have stratigraphy information from well logs look for omitted and duplicated layers. If you have a cross-section look for strata that don't line up or seem to be tilted along a line and imbricate fills/fans, if you have a geologic map look for fault symbols, potential orogenic zones (ie mountains), deformed rocks, oceanic ridges (only for oceans obviously) klippes and fensters (for a reverse fault), and, of course roads mysteriously that stop and start up again 50 feet to the side :P I'm not really sure what you're looking for, it seems like there are a ton of possible answers. 2. A short magnetic history of the earth? I'm pretty that's no longer on the rules, although it may still fall under basic earth history? Either way, I don't really know what to say, except that the Earth's magnetic axis wobbles, and makes a complete loop around the earth's axis every ~5000 years, it can also go on excursions (fun time for the whole magnetic family!), where it wanders significantly from the geographic pole, or inversions, where the magnetic field reverses, every few thousand years. In the the last 76 million years, 171 inversions have occurred. Magnetic history overlayed on geologic time scale: [img]http://s29.postimg.org/n8z6hiarb/Screenshot_2014_05_05_at_6_28_49_PM.png[/img]
First of all, I'm sorry for the ambiguity of my first question haha I was just curious to see what you would put down and how many would overlap with my answers. Everything you mentioned certainly has merit, I would only add a few more possibilities: Slickensides, breccia, polishing/grooving of the rocks, and mylonite. Ugh, I really have to get better at finding/making these questions, I feel like I'm doing you a disservice considering the solid ones you're askingelephantower wrote:Noice!I was worried that boudinage question was a bit too hard...how are the sedimentary environments coming?
1. It depends on the information given. If you have stratigraphy information from well logs look for omitted and duplicated layers. If you have a cross-section look for strata that don't line up or seem to be tilted along a line and imbricate fills/fans, if you have a geologic map look for fault symbols, potential orogenic zones (ie mountains), deformed rocks, oceanic ridges (only for oceans obviously) klippes and fensters (for a reverse fault), and, of course roads mysteriously that stop and start up again 50 feet to the side :P I'm not really sure what you're looking for, it seems like there are a ton of possible answers. 2. A short magnetic history of the earth? I'm pretty that's no longer on the rules, although it may still fall under basic earth history? Either way, I don't really know what to say, except that the Earth's magnetic axis wobbles, and makes a complete loop around the earth's axis every ~5000 years, it can also go on excursions (fun time for the whole magnetic family!), where it wanders significantly from the geographic pole, or inversions, where the magnetic field reverses, every few thousand years. In the the last 76 million years, 171 inversions have occurred. Magnetic history overlayed on geologic time scale: [img]http://s29.postimg.org/n8z6hiarb/Screenshot_2014_05_05_at_6_28_49_PM.png[/img]
Ugh you're killing me hereelephantower wrote:Those slickensides! I actually can't believe I forgot about them... The three environments are (1) undaform for shallow water overlying the shelf, (2) clinoform for the deeper water overlying the slope, and (3) fondoform for the deepest water covering the bottom of the basin (I might have misspoken and said 4 in my original question, sorry). They're not really that important, but still worth knowing. How are those next 4 questions coming?
[img]http://upload.wikimedia.org/wikipedia/commons/7/77/Phacolith.jpg[/img]
1. I'll edit this post with the answer when I get it, my brain hurts right nowelephantower wrote:Noice!I was worried that boudinage question was a bit too hard...how are the sedimentary environments coming?
More questions:1. It depends on the information given. If you have stratigraphy information from well logs look for omitted and duplicated layers. If you have a cross-section look for strata that don't line up or seem to be tilted along a line and imbricate fills/fans, if you have a geologic map look for fault symbols, potential orogenic zones (ie mountains), deformed rocks, oceanic ridges (only for oceans obviously) klippes and fensters (for a reverse fault), and, of course roads mysteriously that stop and start up again 50 feet to the side :P I'm not really sure what you're looking for, it seems like there are a ton of possible answers. 2. A short magnetic history of the earth? I'm pretty that's no longer on the rules, although it may still fall under basic earth history? Either way, I don't really know what to say, except that the Earth's magnetic axis wobbles, and makes a complete loop around the earth's axis every ~5000 years, it can also go on excursions (fun time for the whole magnetic family!), where it wanders significantly from the geographic pole, or inversions, where the magnetic field reverses, every few thousand years. In the the last 76 million years, 171 inversions have occurred. Magnetic history overlayed on geologic time scale: [img]http://s29.postimg.org/n8z6hiarb/Screenshot_2014_05_05_at_6_28_49_PM.png[/img]
1.
Instead of doing the cross-section and parts c and d, determine the minimum net slip of the fault.
2. What are geoblemes and astroblemes (no google please, just your notes)?
3. Name 2 primary igneous and 2 primary sedimentary structures.
4. What feature of thixotropic clay makes it so dangerous?
Knowledge questions don't seem to faze you, so I gave you a lot more this time around.
1. Ptygmatic fold (thanks, binder!) 2. Stereonets! Run! Don't worry I'll ask my partner this one... you can't do this analytically, right? 3. Definitions of competence: 1. responding to my other 4 questions 2. the quality of being resistant to deformation, not ductile 4. Hydrocarbon deposits?
YES I GOT YOU ON THE LAST ONE! Would you like me to tell you? And you can solve it by drawing a diagram with a ruler and protractor as well (number 2). Also, our team as well is dirt poor and we don't go anywhere but someone here was nice enough to send it to me, I'd be happy to do the same for you.elephantower wrote:No I haven't taken the Wright State Invitational (our team is poor and lives in the Southwest, we can't travel to invies). Could you post it on the Test Exchange if you have it? Also, for problems, I need knowledge and analytical (calculations). My partner is taking care of stereonet and other construction (eg 3-point problem) questions, though, so I'd appreciate a few questions to intimidate him withAlso, please no more from the Practical Guide!
answers1. Ptygmatic fold (thanks, binder!) 2. Stereonets! Run! Don't worry I'll ask my partner this one... you can't do this analytically, right? 3. Definitions of competence: 1. responding to my other 4 questions 2. the quality of being resistant to deformation, not ductile 4. Hydrocarbon deposits?