I may be mistaken but there seems to be a trend these days toward ignoring both written and verbal instructions. Now that presents a bit of a dilemma since, to the best of my knowledge, there is no other way to convey instructions. Of course, examples might help, but those also must be either heard or read (and followed!) Nonetheless, in the interest of improving your submissions in any way I can, I've prepared a checklist for your use when submitting assignments.
WARNING: If you ignore this checklist, expect to miss points on every assignment from now on. Maybe I'm getting old and crotchedy, but I no longer have the patience to keep correcting the same simple mistakes, over and over, week after week. If you have a better suggestion about how to obtain compliance, please let me know.
Many entries in the checklist are hyperlinked to an example, so you can be sure you know what is expected of you.
Every assignment should include the following:
Above all else, you might want to ask yourself: "Is this the very best work I can do?" If the answer is "no", then maybe you should ask yourself, "Why am I such a worthless slug?"
Clay Harris
Assignment 2, Encyclopedic dictionary
entry
23 Sept. 2005
Bedding plane
Bedding planes
are two-dimensional surfaces -- they have no thickness; bedding planes
are merely a surface of contact between two sedimentary layers. These layers
may be laminations – having a thickness less than 1 cm – or beds, which
are thicker than 1cm. Bedding planes form when conditions change during
sediment deposition by gravity, wind, water, or ice. These conditions include
water velocity, sediment volume, or grain size. Thus, the character of
sediment accumulation changes and a bedding plane may form.
Bedding planes
often host features, called bedding plane markings, which occur either
at the base of a bed or its top. Those at the base typically form as a
new layer accumulates; for example, groove marks may develop as a pebble
gouges out sediment from a stream bed. Bedding plane markings at the top
of a bed generally form after sedimentation ceases; for example,
mud cracks form by desiccation of exposed mud.
If you trace
any bedding plane laterally, you will find that it eventually ends in one
of three ways: (a) erosion destroyed the over and underlying beds as well
as the bedding plane; (b) the two beds become one; (c) one of the beds
involved gradually thins and then disappears.
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