describe an angular unconformity, a disconformity, and a nonconformity. What does each indicate aboutpastevent
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An unconformity is a gap in time in rock layers, where erosion occurs while deposition slows or stops. The rocks above an unconformity are younger than the rocks beneath (unless the sequence has been overturned). An unconformity represents time during which no sediments were deposited and the local record for that time interval is missing and geologists must use other clues to discover that part of the geologic history of that area. The interval of geologic time not represented is called a hiatus. There are three types of unconformities: disconformity, nonconformity, and angular unconformity.\n\nDisconformity\nAn unconformity between parallel layers of sedimentary rocks which represents a period of erosion or non-deposition.\n\nNonconformity\nAn unconformity exists between sedimentary rocks and metamorphic or igneous rocks when the sedimentary rock lies above and was deposited on the pre-existing and eroded metamorphic or igneous rock.\n\nAngular Unconformity\nAn unconformity where horizontally parallel strata of sedimentary rock is deposited on tilted and eroded layers that may be either vertical or at an angle to the overlying horizontal layers. The whole sequence may later be deformed and tilted by further orogenic activity.\n\nRetrieved from "http://en.wikipedia.org/wiki/Unconformity"
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What symbol is used to indicate mapping?\n--usually an arrow\n\nWhich transformation turns a figure?\n--rotation\n\nWhich transformation slides a figure?\n--translation\n\nWhat does a dilation do to a figure? \n--scales it up - kinda like zooming in or making an enlargement\n\nName the three isometries.\n--rotation, translation, reflection\n\nWhich transformation is not an isometry?\n--dilation\n\nExplain a similarity transformation.\n--A similarity transformation changes figures into similar figures - pretty much all of the above transformations
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Spiral, lenticular, elliptical and irregular\n\nSee the link
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Slickenlines will give a direction of slip, but as you have probably thought out, that still has two possible interpretations. It isn't always easy, but there are several things you may observe that will help.\n\nSlickensides will also develop a series of small steps that show the sense of movement. These are somewhat perpendicular to the fault movement and the steps will be the trailing edge of the movement direction. \nHere is a picture, where the top (missing portion) side moved to the left. \nhttp://www.geo.cornell.edu/geology/class...\nHere are several other illustrations of these steps:\nhttp://www.geo.cornell.edu/geology/class...\n\nDrag folds will also help you determine the sense of movement. These folds are distortions of the bedding due to shearing along the fault. They are convex toward the direction of slip, with the exception of rollover anticlines along listric normal faults. To describe it another way, the shear will form a 'cup-like' pattern near the fault in the bedding, the bottom of the 'cup' will point toward the direction of movement. If on the upper side of the fault your 'cup' points downward, it should be a normal fault, and if this 'cup' points upward on the upper side of the fault, it is likely a reverse fault. \n\nUsing stratigraphic layers will often not get you much further than the slickenlines, giving you two possible directions. But, in some outcrops you can look at the topmost part of the fault and also see some evidence of the sense of movement by observing the most recent deposition or the thickness of the soil layer over the fault blocks. Where the fault blocks have been eroded away equally on both sides this may not help. \n\nIn other instances you may have to do more mapping and examine other faults in the area before you can make a conclusion. If you know the area is extensional, then you have a hypothesis to work with. The best idea is to always check as many kinds of evidence as you can find before you make a conclusion.
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It's the axis stuff rotates around and if you stop it from rotating at one random point, it will look like any other random point.  For instance, if you had a circle, as long as your axis went through the center, it's an axis of symmetry because no matter how you rotate the circle around that axis, it will look the same.  But if you drew a line through the circle that didn't go through the center, and rotated your circle, it would wobble back and forth - non-symmetrically.
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Originality\n\nSincerity\n\nStructure\n\nGrammar\n\nSpelling\n\nVoice\n\nPunctuation\n\nProse\n\nConclusion\n\nThe Unexpected
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It's been too long for me.\n\nSample many definitions. Go to MATHWORLD.COM (lower case)\n2 geometric figures are CONGRUENT when one gets transformed into the other by isometry.\n\nStay with it.\n\nGRIZZ
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a·nom·a·ly    ( P )  Pronunciation Key  (-nm-l)\nn. pl. a·nom·a·lies \nDeviation or departure from the normal or common order, form, or rule. \nOne that is peculiar, irregular, abnormal, or difficult to classify: “Both men are anomalies: they have... likable personalities but each has made his reputation as a heavy” (David Pauly). \nAstronomy. The angular deviation, as observed from the sun, of a planet from its perihelion.\n\n\nwatch ur spelling
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Think about it.  If you have an angle drawn on a sheet of paper and you rotate one segment, will the length of the segment still be the same?  Yes, all you're doing is changing its position, the length remains the same.  \nWill the measure of the angle remain the same?  Of course not, by rotating one segment you're automatically changing the angle from it to the other segment.  \nFinally, if you rotate a segment, is it still oriented the same?  No way!  You just changed its position, how can it still be oriented the same way?
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http://focus.ti.com/lit/ml/slup117/slup117.pdf
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You should be able to select the constaint in the outliner.  Select it and delete it.  If that doesnt work, i hope you saved recently.
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You may be talkig about a square, sine, and sawtooth (triangle) waveforms. They look like their names imply on an oscilloscope. They have no special significance other than they are descriptive of the type of AC wave they describe. It is like asking what are the different colors and what are their significance?
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Originality=0\nUnderstanding=0\nArgument=0\nConclusion=0\n\nOverall=0\n\nSummary: Liberal political science fiction. No facts, no point, no nothing.
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It is Widmanstatten Structure, not Wandermanstateen, and is\na structure characterized by a geometrical pattern resulting from the formation of a new phase along certain crystallographic planes of the parent solid solution. The orientation of the lattice in the new phase is related crystallographically to the orientation of the lattice in the parent phase. The structure was originally observed in meteorites but is readily produced in many other alloys with certain heat treatment.\n\n\nU can go to find some links with the right spelling.\n:)
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rejection\nburing alive\ndrowning\nan unexpected death in general\nconformity
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Collective inertia towards innovation. What is a widely used mistake today is the standard tomorrow. Try to worry more about the quality of the writing than the attention to grammatical "rules."
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I'll help you with type of characterization first\nthis means what the character is like ie static dynamic round, static and flat. In a short story there is rarely room for more than one dynamic character\nfigure of speech has a few forms similies, metaphors and exageration\nmetaphors compare one thing without using like\nsimilies are sentences that use like\nexageration.......well you know exagerating stuff I'm so hungry I can eat a horse\nelements of literature are the following\nsetting\nplot \ncharacterization\nmethods of characterization\npoint of view\nconflict\ntheme\n tone\nsorry I don't know the symbol thing though!!\nhope I helped you\nif you need more help you can e mail me