Friday, December 16, 2005

Many people will start typing something, then edit it, and then retype it, and reedit it, and hocus pocus the post comes up on their blog. The there are people like me, who think of some topic that makes them angry and then just lets loose. Rarely do they edit their posts and normally it's full of typos and the writing doesn't turn out quite as clean and logically sound as one might expect. I have typed posts out before and heavily edited them (I do that with every The Scheister article (don't tell anyone)), but normally I type what I want to say on the fly (this post, for instance).

I hope everyone contributed to the Lutheran Carnival this cycle. If you haven't, why not?

There are many posts here on the Lutheran blogsphere where I about wanted to pound my head in with a hammer because I, for some reason, can't figure out what the author is talking about. At times, I wish I was better read in the classics and literature. I wish I was better read in general. Much of my theological education started only seven years ago when I finally got a Book of Concord as a graduation present.

The fact is, however, English is not my strong suit and it never will be. When people tell me there is some deep significance to a book, I kind of scratch my head and wonder because, most of the time, I see the book in question as a good story and am clueless as to what I was supposed to see. This is from a kid who spent considerable time in parochial schools.

OK, to give those whose blogs sometimes speak above my level an example of what I am talking about, let me quote from a paper I am currently reading.

The direction in which synorogenic foreland carbonate platforms backstep is dependent on the orientation of the carbonate platform margin and reef facies tracts with respect to an advancing orogenic wedge. If a platform margin trend is subparallel to the axis of the orogenic wedge and its adjacent foredeep, the entire margin will backstop as the orogenic wedge advances toward the platform. (citation omitted). In contrast, if the platform margin is oriented at a high angle to the orogenic wedge and foredeep axis, backstepping will be highly diacronous. (citation omitted).
Quoted from Dorbrek, S. L., 1995, Synorogenic carbonate platforms and reefs in foreland basins: controls on stratigraphic evolution and platform/reef morphology, in Dorbrek, S. L. and Ross, G. M. eds., Stratigraphic evolution of foreland basins: Tulsa, SEPM Special Publication 52, p. 141


In case you are wondering, yes, I completely understand the above paragraph. Of course, context helps but I would be violating all sorts of copyrights if I did that. I am going to go finish this paper (it is quite interesting and riveting to me)and call my girlfriend soon.

No comments: