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If you need a speaker for your club or function give me a call. I agree that people are generally rude, but that is probably because there are too many people on the streets and too much work pressure—so no one has time to stop and say Hi; and by being rude atleast they are not two-faced. Instead they paid for the cush retirements of all the overpaid teachers, police officers, and bureaucrats. Yes, I have thoroughly enjoyed reading your reports, as well as seeing the successes of others. Resting on the bedrock and extending under nearly all of Long Island is a massive wedge of Cretaceous sediments sands, clays and gravels. On Friday I was back in Heampstead harbor thowing pencil poppers, but only managed 2 bass.

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Welcome to our calendar of events for the Jersey Shore. Come back often to get updates about the latest Jersey Shore eventshappenings, concerts, festivals, sports, children activities and more. Also, check out the Jersey Shore Vacations blog for up to date news about what's happening at the shore. Benefits Special Olympics New Jersey. Noon-7pm in the White St parking lot.

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The surface of Long Island is made up of many varied and interesting landforms. Each natural land feature originated through the action of some past or present geologic process. On Long Island these processes can be grouped into three categories - pre-glacialglacial and post-glacialdepending on whether they occurred before, during or after the advance of a continental glacier onto the Island. Pre-glacial geologic events in the Long Island include the formation of the ancient over million year old metamorphic bedrock that forms the foundation upon which Long Island rests, and the deposition of sands and clays on this bedrock 70 million years ago, during the late Cretaceous period. Surface exposures of the bedrock are widespread in Manhattan and the Bronx but are limited on Long Island to small outcrops in northwestern Queens. The bedrock slopes down to the south and east beneath the rest of Long Island and therefore does not form any significant landforms here. Resting on the bedrock and extending under nearly all of Long Island is a massive wedge of Cretaceous sediments sands, clays and gravels. This wedge is over 2, feet thick under Fire Island, but it thins towards the north shore and the western end of the Island to pinch out under Long Island's Sound, western Queens and Brooklyn. The top surface of the Cretaceous reaches elevations above sea level over an extensive area of northern Nassau and northwestern Suffolk counties.

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A haven for boaters, bathers, and sport fishermen. A source of endless fascination for kids. Its calm surface extends as far as the eye can see eventually narrowing down to almost nothing at the Smith Point Bridge in Moriches. It stretches about 6 more miles beyond the bridge and into Amityville before its name changes to South Oyster Bay.