Established | 2019 |
---|---|
Location | 99 Main St, Bethel, Maine |
Coordinates | 44°24′28″N70°47′19″W / 44.4077°N 70.7887°W |
Type | Geology museum |
Website | mainemineralmuseum |
The Maine Mineral and Gem Museum (MMGM) is a geology museum located in Bethel, Maine. [1] [2] It displays a collection of rocks, minerals, and meteorites.
The Maine Mineral & Gem Museum celebrates Earth and cultivates critical thinking through education, research and dynamic exhibits—all designed to inspire visitors about Maine's geologic history, pegmatite mining, and our planet's place in the solar system.
The museum was formed from the possessions within Perham's Maine Mineral Store, which was founded in 1919. Following the store's closure in 2009, Massachusetts-based philanthropists Lawrence Stifler and Mary McFadden purchased the Perham collection. The Maine Mineral and Gem Museum then opened in 2019. [3]
As of 2021, the museum holds 57,781 specimens, with 37,940 of those being minerals. [4] Notable specimens contained by the museum are:
The MMGM collection is home to more than 38,000 superlative mineral specimens, housing over 15,000 from Maine which includes more than 300 exceptional gemstones of exquisite quality. The 15,000sq ft museum has four galleries and nineteen permanent exhibits showcasing the world's most comprehensive collection of Maine minerals, as well as Earth's foremost collection of meteorites from the Moon and Mars. Additionally, the MMGM's active research laboratory supports scientific exploration of both minerals and meteorites. The MMGM houses approximately 6,000 extraterrestrial rocks (originating from the Moon, Mars, and Asteroid Belt) that are showcased in the Stifler Collection of Meteorites-a state of the art gallery that showcases the internationally renowned meteorite collection featuring extraterrestrial rocks from Mars and the asteroid belt, and holds more meteorites from the Moon than every national history museum in the world--combined. [8]
The William “Skip” Simmons Research Laboratory at MMGM is led by a world-class team of scientists and researchers from Maine and around the globe. Through the use of cutting edge technology and ground-breaking research, the lab is expanding the fields of mineralogy, petrology, pegmatology, and cosmochemisty every day.
Through collaboration with academic institutions and researchers from around the globe, MMGM’s team of researchers have co-authored and presented over 100 scientific studies in the past decade and written over 500 peer-reviewed publications throughout their career.
MMGM and the MP2 Research Team offer an annual opportunity to study granitic pegmatites with expert pegmatologists in the heart of western Maine at the Maine Pegmatite Workshop.
The Maine Pegmatite Workshop brings participants through a hands-on, comprehensive, and in-depth educational experience, presenting current information and theories about pegmatite paragenesis, mineralogy, and petrology. The workshop encourages open discussion and one-on-one information exchange side-by-side with some of the top pegmatologists in the world.
The Maine Pegmatite Workshop curriculum delves deeply into a broad array of pegmatite-focused topics including, but not limited to: [9]
In 2014, Maine Lapidary and MMGM Founding director and trustee emeritus, Robert F. Ritchie, MD, donated to the museum more than 800 stone spheres and the lapidary equipment that he used to cut and polish them. His sphere machine is a prominent part of the museums lapidary exhibit.
Currently, the Robert F. Ritchie Lapidary Studio at the Maine Mineral and Gem Museum is overseen by exhibit specialist and studio manager, Martin Roberts. Roberts is most often found in the studio, making spheres out of metamorphic, sedimentary, and igneous rock, and even meteorites. [10]
A pegmatite is an igneous rock showing a very coarse texture, with large interlocking crystals usually greater in size than 1 cm (0.4 in) and sometimes greater than 1 meter (3 ft). Most pegmatites are composed of quartz, feldspar, and mica, having a similar silicic composition to granite. However, rarer intermediate composition and mafic pegmatites are known.
The mineral olivine is a magnesium iron silicate with the chemical formula (Mg,Fe)2SiO4. It is a type of nesosilicate or orthosilicate. The primary component of the Earth's upper mantle, it is a common mineral in Earth's subsurface, but weathers quickly on the surface. For this reason, olivine has been proposed as a good candidate for accelerated weathering to sequester carbon dioxide from the Earth's oceans and atmosphere, as part of climate change mitigation. Olivine also has many other historical uses, such as the gemstone peridot, as well as industrial applications like metalworking processes.
Orthoclase, or orthoclase feldspar (endmember formula KAlSi3O8), is an important tectosilicate mineral which forms igneous rock. The name is from the Ancient Greek for "straight fracture", because its two cleavage planes are at right angles to each other. It is a type of potassium feldspar, also known as K-feldspar. The gem known as moonstone (see below) is largely composed of orthoclase.
A Martian meteorite is a rock that formed on Mars, was ejected from the planet by an impact event, and traversed interplanetary space before landing on Earth as a meteorite. As of September 2020, 277 meteorites had been classified as Martian, less than half a percent of the 72,000 meteorites that have been classified. The largest complete, uncut Martian meteorite, Taoudenni 002, was recovered in Mali in early 2021. It weighs 14.5 kilograms and is on display at the Maine Mineral and Gem Museum.
In geology, the crust is the outermost solid shell of a planet, dwarf planet, or natural satellite. It is usually distinguished from the underlying mantle by its chemical makeup; however, in the case of icy satellites, it may be distinguished based on its phase.
Amateur geology or rock collecting is the non-professional study and hobby of collecting rocks and minerals or fossil specimens from the natural environment. In Australia, New Zealand and Cornwall, the activities of amateur geologists are called fossicking. The first amateur geologists were prospectors looking for valuable minerals and gemstones for commercial purposes. Eventually, however, more people have been drawn to amateur geology for recreational purposes, mainly for the beauty that rocks and minerals provide.
An achondrite is a stony meteorite that does not contain chondrules. It consists of material similar to terrestrial basalts or plutonic rocks and has been differentiated and reprocessed to a lesser or greater degree due to melting and recrystallization on or within meteorite parent bodies. As a result, achondrites have distinct textures and mineralogies indicative of igneous processes.
Moon rock or lunar rock is rock originating from Earth's Moon. This includes lunar material collected during the course of human exploration of the Moon, and rock that has been ejected naturally from the Moon's surface and landed on Earth as meteorites.
Troilite is a rare iron sulfide mineral with the simple formula of FeS. It is the iron-rich endmember of the pyrrhotite group. Pyrrhotite has the formula Fe(1-x)S which is iron deficient. As troilite lacks the iron deficiency which gives pyrrhotite its characteristic magnetism, troilite is non-magnetic.
Whitlockite is a mineral, an unusual form of calcium phosphate. Its formula is Ca9(MgFe)(PO4)6PO3OH. It is a relatively rare mineral but is found in granitic pegmatites, phosphate rock deposits, guano caves and in chondrite meteorites. It was first described in 1941 and named for Herbert Percy Whitlock (1868–1948), American mineralogist and curator at the American Museum of Natural History in New York City.
Kaidun is a meteorite that fell on 3 December 1980 on a Soviet military base near what is now Al-Khuraybah in Yemen. A fireball was observed travelling from the northwest to the southeast, and a single stone weighing about 2 kilograms (4.4 lb) was recovered from a small impact pit. It has been suggested that Kaidun originated from the Martian moon of Phobos, but this is disputed.
The Rice Northwest Museum of Rocks and Minerals is a non-profit museum in Hillsboro, Oregon, United States. Located just north of the Sunset Highway on the northern edge of Hillsboro, the earth science museum is in the Portland metropolitan area. Opened in 1997, the museum's collections date to the 1930s with the museum housed in a home built to display the rock and mineral collections of the museum founders. The ranch-style home is listed on the National Register of Historic Places, the first of its kind listed in Oregon. In 2015 the museum became a Smithsonian Affiliate museum.
Mineral collecting is the hobby of systematically collecting, identifying and displaying mineral specimens. Mineral collecting can also be a part of the profession of mineralogy and allied geologic specialties. Individual collectors often specialize in certain areas, for example collecting samples of several varieties of the mineral calcite from locations spread throughout a region or the world, or of minerals found in pegmatites.
Mars may contain ores that would be very useful to potential colonists. The abundance of volcanic features together with widespread cratering are strong evidence for a variety of ores. While nothing may be found on Mars that would justify the high cost of transport to Earth, the more ores that future colonists can obtain from Mars, the easier it would be to build colonies there.
The Mineral and Lapidary Museum of Henderson County is a non-profit, volunteer-run museum in Hendersonville, North Carolina, United States, founded in 1997 at 400 North Main Street in the middle of the city's Historic District.
The composition of Mars covers the branch of the geology of Mars that describes the make-up of the planet Mars.
The Tissint meteorite is a Martian meteorite that fell in Tata Province in the Guelmim-Es Semara region of Morocco on July 18, 2011. Tissint is the fifth Martian meteorite that people have witnessed falling to Earth, and the first since 1962. Pieces of the meteorite are on display at several museums, including the Museum of Natural History of Vienna and the Natural History Museum in London.
John Sinkankas was a Navy officer and aviator, gemologist, gem carver and gem faceter, author of many books and articles on minerals and gemstones, and a bookseller and bibliographer of rare books.
This is a glossary of terms used in meteoritics, the science of meteorites.
Yamato 000593 is the second largest meteorite from Mars found on Earth. Studies suggest the Martian meteorite was formed about 1.3 billion years ago from a lava flow on Mars. An impact occurred on Mars about 11 million years ago and ejected the meteorite from the Martian surface into space. The meteorite landed on Earth in Antarctica about 50,000 years ago. The mass of the meteorite is 13.7 kg (30 lb) and has been found to contain evidence of past water alteration.