Showing posts with label deep. Show all posts
Showing posts with label deep. Show all posts

Sunday, April 15, 2018

From Deep . . .

. . . inside . . .


Like house and soldiers
Checkers and chess
My heart and soul
Paid dearly their dues
Learning we called it
and learning it was
But I itched to be finished
And to make my own news

Was not really concerned
Of the what and the how
Being preoccupied
With the here and the now
Everyone I encountered
Was informed of my view
No holds barred
I bombarded not few

Now lo many an issue transpired
I have seen countless things
Have lived well was inspired
Maybe you do not know me
From exploits derrynge do
But I've devoted my all
To endeavors unfew
It isn't fatigue or exhaustion I feel
It's just time for the new


Heart Purge Three
©2017 Raymond M. Jozwiak



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Thursday, November 7, 2013

Finger. . .


. . . lakes


(from http://www.priweb.org/ed/finger_lakes/nystate_geo3.html)
The Finger Lakes consist of 11 long, narrow, roughly parallel lakes, oriented north-south as fingers of a pair of outstretched hands. The southern ends have high walls, cut by steep gorges. Two of the lakes (Seneca and Cayuga) are among the deepest in North America and have bottoms below sea level. These lakes all formed over the last two million years by glacial carving of old stream valleys. Ithaca is located at the south end of Cayuga Lake, the longest and the second deepest of the Finger Lakes. Cayuga is 38.1 miles long and 435 feet deep (53 feet below sea level) at its deepest spot. The actual depth of carved rock is well over twice as deep, but it has been filled with sediments; there may be as much as 1000 feet of glacial sediment in the deep rock trough below the lakebed.

The Finger Lakes originated as a series of northward-flowing rivers that existed in what is now central New York State. Around two million years ago the first of numerous continental glaciers moved southward from the Hudson Bay area, initiating the Pleistocene glaciation, commonly known as the "Ice age."

The most obvious evidence left by the glaciers are the gravel deposits at the south ends of the Finger Lakes called moraines and streamlined elongated hills of glacial sediment called drumlins. Moraines are visible south of Ithaca at North Spencer, along Route 13 west of Newfield, and near Willseyville. Drumlins are visible northeast of Ithaca at the northern end of Cayuga and Seneca lakes in a broad band from Rochester to Syracuse.


Keuka
©2013 Raymond M. Jozwiak





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