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JOHN G. JACKSON

Answer
Born on September 8, 1818, in what is known today as the Dixon-Jackson House, J.G. Jackson studied at the Westtown Boarding School beginning at age 14. In his 20s, he began teaching science and astronomy at Westtown. Jackson became a surveyor’s apprentice when he was 21, mastering the profession while working for the government in Ohio. By age 30 (1848) Jackson was supervising the family’s Hockessin saw mill operation, doing surveying within New Castle County, supervising the daily operations of the limestone and marble quarries on the family’s property, and overseeing construction of a new home for his family northeast of Valley and Southwood roads.
John G. Jackson became a notary public for New Castle County in 1857 at age 39. In November 1864, Jackson successfully won the election to become a State Representative for New Castle County in the 73rd Delaware General Assembly for two years (January 3, 1865 to January 1, 1867). Jackson served as Chief Engineer for the Wilmington & Western Rail Road’s construction between 1870 and 1872, and its route remains a testament to his skills as a surveyor and engineer. In 1880, at age 62, Jackson began to embrace retirement by selling the quarry business. Jackson continued his surveying activities in later years as he applied for a patent related to surveying in June 1888. Jackson was awarded Patent 392,124 on October 30, 1888, for a ‘Spirit-Level’.
Jackson was an avid astronomer, and in 1837 he worked out the calculations for the next transit of Venus (a transit is when the orbital planes of Earth and Venus are aligned such that from the daylight side of Earth one may observe Venus as a black dot moving across the sun). When Jackson made the initial calculations, only two individuals had ever observed Venus transit the sun (in 1639). One must remember that humans did not know the precise orbits (elliptical and not circular) of Venus and the Earth or their mean distances from the sun.
Jackson used his telescope, observational skills, and math knowledge to calculate current positions and then to reliably predict the future orbits of the Earth and Venus circling the sun. Adding to the complexity is the fact that the orbital planes of the two planets are different (3.8 degrees), the frequency of Earth-Venus-Sun alignment occurrence differs (105.5 years, 8 years, 121.5 years, 8 years before repeating), and the calculations are done with only a pencil and paper by kerosene lamps!
The 1874 Venus transit was not visible in North America (it was visible in eastern China, Australia, Japan, Indonesia). Jackson was rewarded for his efforts on December 6, 1882, when he was able to document, along with other noted astronomers across North America, the transit of Venus as he and others had predicted 37 years earlier! Jackson’s work is documented in multiple astronomy periodicals of the time, and his involvement is noted in Congressional records. Jackson owned a 6-inch reflecting telescope that he most likely made himself. This would have been a large telescope for a private individual as the best observatories around the world had telescopes of the size of Mt. Cuba Observatory’s 24-inch reflector in the 1880s.
J.G. Jackson is also documented as having observed “clouds” on the moon on multiple occasions. Galileo Galilei’s improvements to the telescope in the early 1600s allowed better viewing of the moon. As far back as February 1672, a “nebulous appearance” had been reported in the Mare Crisium region of the moon by Giovanni Domenico Cassini. From Cassini’s first reporting until Jackson’s time, dozens of reported sightings had occurred, with some reporting a purple color to the cloud or fog.
As part of America’s preparations for going to the moon, in 1968 NASA released a Chronological Catalog of Reported Lunar Events documenting 580 observances over nearly 300 years of cloud-like phenomena on the moon. By the early 1900s, it was well accepted that the moon did not have an atmosphere. Continued study of the moon concludes that the “clouds,” bright flashes, and other lunar phenomena are more than likely the result of out-gassing from the moon’s crust, impacts of space debris with the surface, or similar causes. Only since the Apollo flights of the 1970s have we learned the moon does have what can be considered an atmosphere (ten trillion times thinner than Earth composed of atoms of sodium, potassium, helium, argon, ammonia, methane, and carbon dioxide).
PLEXI CAR
An alternate to silica-based glass is acrylic glass. Technically known as Poly-Methyl-MethAcrylate (PMMA), we commonly refer to the material generically as plexiglass. Developed by Rohn & Haas Company commercially in 1933, their Plexiglas product was trademarked in Germany as the world’s first clear acrylic material. Imperial Chemical Industries Ltd. (ICI) registered the product in the UK at about the same time as “Perspex.” In the U.S., E.I. du Pont trademarked Lucite as their acrylic glass product offering. Other companies have trademarked names such as R-Cast, Optix, and Cyrolite.
In 1939, for the World’s Fair, the car below was featured having its exterior body panels fabricated from Rohm & Haas Plexiglas. It was advertised as the first “transparent car” in America. Who was the manufacturer of the automobile pictured, and which major automotive manufacturer showcased the vehicle during the fair?
Answer
Often called the PlexiPontiac, or the Pontiac Ghost Car, it is a 1939 Pontiac Deluxe Six. It was built as a collaboration between General Motors, Pontiac, and Rohm & Haas for the GM “Futurama” exhibit and was part of the “Highways & Horizons” display. Built on a 120-inch wheelbase, Pontiac four-door Touring Sedan framework and chassis, the metal structural components were copper plated while the car’s accent hardware was chrome plated. Black rubber moldings were changed to white rubber as were the tires, for contrast. The engine used was a 222.7-cubic-inch L-head six-cylinder that generated 85 brake horsepower for the three-speed manual transmission.
Costing $25,000 to build, the odometer displays only about 100 miles of driving! After being one of the must-see highlights at the World’s Fair, the car toured the U.S. before becoming a feature attraction at the Smithsonian Institute for a number of years. Upon leaving the Smithsonian in 1947, it was displayed in several Pennsylvania dealerships. It was purchased in the early 1970s by a private owner, who had it restored. Sold to another private owner in the late 1970s, it was again sold to a private owner in the 1980s. In July 2011, it was auctioned by RM Auctions for $308,000.
A second car was built after the Ghost Pontiac on the Pontiac Torpedo Eight chassis for the Golden Gate Exposition. It too toured the country, but its status is unknown.
RARE ITEM
The rare item pictured has been awarded a National Register of Historic Places listing. It is located on the border between Delaware and Maryland in Delmar but originally found use in northern Delaware as well as 25 miles away in Hurlock, Maryland. After serving some of its life in Cape Charles, Virginia, it has been returned to Delaware. What is the pictured item called, and how was it used?
Answer
The item pictured is a railroad Highball Signal dating from the earliest railroads that operated on the DelMarVa Peninsula. From the Delmar Highball Signal’s National Register Listing;
The term highball, meaning a fast train, or permission for a train to proceed at full speed, derives from this type of signal. A highball signal was a white sphere mounted on a pole next to the railroad tracks. If the track was clear ahead, the signal attendant would raise the ball to the top of the pole by means of a pulley. If the track was not clear, he would lower the ball so that it would not be visible to the engineer of an oncoming train; hence, the term highball came to be synonymous with a clear right-of-way. Positioned as shown in the image, at the midpoint of the pole, the signal indicated the engineer was to proceed ahead slowly with caution.
Highball signals were frequently mounted near stations or at section boundaries. The design of highball signals varied among the railroads; some were equipped with a black ball that would replace the white one when the track was not clear. Some signals, like the one at Delmar, were provided with a box into which the ball was lowered when the track was not clear. Some railroads constructed the ball with glass windows such that it included a kerosene font and burner and could be lit at night for better visibility. Other types of signal, notably the semaphore and the three-light electrical signal, eventually replaced the highball. The highball at Delmar is a steel sphere mounted on a wooden post, which is raised and lowered by of a chain hoist. It is no longer used to direct railroad traffic, but is maintained as a public exhibition in a park near the railroad.
The highball signal at Delmar is one of the last survivors of a type of traffic control that was in use before the advent of modern semaphore signals. The origin of the highball is unknown, but it probably was invented during the railroad expansion period of the 1840’s. As a signal, it is quite primitive, since it can convey only one piece of information: whether the track is clear or not. Modern signaling devices can transmit a variety of data to the engineer of an oncoming train. The last highball signal on a class 1 railroad in America was in operation at the interchange point between the Pennsylvania and Reading railroads near Wilmington Delaware, a few years ago; the highball was used at that point because the electronic control systems of the two railroads ended short of the interchange track and manual signaling was necessary.
The Delmar highball signal was originally in service at New Castle, Delaware, and then at Hurlock, Maryland. It was displayed for a time at Cape Charles, Virginia, and then was moved to Delmar, Delaware for display during the town’s centennial in 1959. It is maintained as a permanent exhibit by the town of Delmar, Delaware.
THE FIRST TRAIN ROBBERY
The books of the late 1800s and the movies of the mid-1900s have tended to embellish the typical train robbery of the the late 1800s. Riding alongside a moving train and jumping aboard was a dangerous proposition. It was far easier for robbers to buy a ticket and board as a paying passenger to gain access to a train to be robbed. A few robbers could take over a train and bring it to a stop at a prearranged location where other gang members could board and not only relieve passengers of their gold jewelry and other valuables but dynamite safes in baggage or box cars.
NATURAL ICE HARVESTING
This past summer, as part of the Eastern Invitational Steam Car Tour, tour participants had the opportunity to visit the Antique Ice Tool Museum in West Chester, PA. The old barn, now converted into a museum, is full of artifacts of the 1800s, when natural ice was harvested from local creeks and ponds and stored over the summer months for consumption and for keeping food cold. Ice harvesting of America’s ponds and lakes became one of the nation’s biggest export incomes during the late 1800s, when more than two million tons of ice were harvested annually. When ammonia refrigeration plants began making year-round ice at the very end of the 19th century, more than 20 million tons of natural-formed ice were being harvested or produced commercially.
If one researches outdoor temperatures in the late 1800s, you will find weeks of below-freezing temperatures occurred during winter months in our area. This was more than sufficient “cold” to freeze the Red Clay Creek to a sufficient thickness that it could be harvested for ice. In February 1887, the Delaware General Assembly authorized the formation of the Greenbank Ice Company of Marshallton, DE, for the harvesting of ice on the Red Clay Creek. The Baltimore & Ohio Railroad is documented by the Evening Journal as harvesting 12-inch thick pond ice held behind the Greenbank Mill’s dam on January 14, 1893. On January 8, 1900, the Evening Journal documented that 6- to 8-inch thick ice was being harvested from the large lake at Brandywine Springs Amusement Park. The Mitchell family harvested ice in winter months for storage in the ice house alongside the farmhouse and behind the creamery, which could be used for keeping milk cold. No doubt the Marshalls harvested ice for storage from the tranquil waters behind their mill dams before the age of refrigeration.
Does anyone still harvest ice naturally in the U.S., and if your answer is “yes,” where is it done?
Answer
Natural ice is routinely harvested in Maine, Montana, New Hampshire, and Wisconsin as well as Ontario, Canada, at least in 2019. The 190-year-old Maine ice harvest is performed by the Thompson Ice House Harvesting Museum. Around 7 tons of ice is harvested in mid-February and stored until the July ice cream social, where the ice is used to make ice cream and for snow cones.
The best known and perhaps largest natural ice harvest for keeping foods cold occurs annually at Squam Lake near Holderness, New Hampshire. Once a commercial ice operation first operated in 1897, today the ice is harvested using more modern methods for use by the Rockywold-Deephaven Camps, a resort community open only during the summer months. Roughly 3,600 ice blocks weighing 120 to 150 pounds (roughly 16″ x 19″ by the ice’s thickness somewhere between 12″ and 15″) are harvested in mid-January to mid-March each year for storage in one of two ice houses. The ice is used during the summer months to fill the “ice boxes” located in each of the cottages on the resort property. For more information visit their website.