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The intermediate School, Haddam-Killingworth Middle School, is located in the town of Killingworth and houses 5th grade - 8th grade.
Initially, the plan was to have the old Middle School complex become a part of the Haddam-Killingworth HS, the old Middle School part of the complex was converted into a district-run daycare facility, the main offices of the district administration, and also houses the local state trooper's office.
In the town, the population is spread out with 24.7% under the age of 18, 5.0% from 18 to 24, 30.2% from 25 to 44, 30.4% from 45 to 64, and 9.7% who are 65 years of age or older.
The median age is 40 years, for every 100 females there are 102.0 males.
As of the census of 2000, there are 7,157 people, 2,701 households, and 2,101 families residing in the town, the population density is 162.5 inhabitants per square mile (62.8/km²).
(1954): Pegmatite Investigations 1942-45 New England; USGS Professional Paper 255: 333-338.; Stugard, Frederick, Jr.
(1958): Pegmatites of the Middletown Area, Connecticut. Description: Coarse tabular aggregates, commonly with terminations in interstitial spaces, forms much of the matrix of the up to 45-foot-thick plagioclase-quartz intermediate zone that hosts much of the interesting mineralization such as morganite, elbaite, spodumene, lepidolite, montebrasite, K-rich albite, cookeite, columbite, tantalite, wodginite, quartz crystals, etc. Description: As generally small crystals in the outer zones of the pegmatite, but also massive concentrations mixed with fluorapatite, zinnwaldite/masutomilite, elbaite and columbite-(Fe) in cleavelandite.
Reference: Cameron, Eugene N., Larrabee, David M., Mc Nair, Andrew H., Page, James T., Stewart, Glenn W., and Shainin, Vincent E. State Geological and Natural History Survey Bulletin 51.; Schooner, Richard. Gemmy crystals in this assemblage confirmed using Raman spectroscopy typically partially replaced by waxy yellow fine-grained muscovite (also confirmed by Raman).
(1954): Pegmatite Investigations 1942-45 New England; USGS Professional Paper 255: 333-338. Also, in the host metamorphic rocks as a component of "coticule" rock.