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Weston meteorite (incl Easton; Trumbull; Fairfield), Easton (Weston), Fairfield County, Connecticut, USAi
Regional Level Types
Weston meteorite (incl Easton; Trumbull; Fairfield)Strewn Field
Easton (Weston)- not defined -
Fairfield CountyCounty
ConnecticutState
USACountry

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Latitude & Longitude (WGS84):
41° 15' 55'' North , 73° 16' 35'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Most of the fragments of this meteorite were found within the boundaries of the modern town of Easton, which was the eastern part of the town of Weston until 1845, when it became a separate town. Other finds are in the towns of Trumbull and Fairfield, which were already separate towns in 1807.
Köppen climate type:
Mindat Locality ID:
62857
Long-form identifier:
mindat:1:2:62857:1
GUID (UUID V4):
0


First witnessed fall in the United States, December 14, 1807.
Olivine-Bronzite Chondrite (H4; S3; W0).
Approximate recovered mass 149.7 kg; Several stones, largest 90.7 kg (fragmented)


NOTE: Most of the fragments of this meteorite were found within the boundaries of the modern town of Easton, which was the eastern part of the town of Weston until 1845, when it became a separate town. Other finds are in the towns of Trumbull and Fairfield, which were already separate towns in 1807 (King and Petruny, 2008). The locality marker is placed at the main recovery site in modern day Easton.

Witnesses saw and heard the early morning “red fire ball” along its generally north-to-south path in southern Vermont, western Massachusetts, and Connecticut. Many sonic booms were heard, though having no experience with that modern phenomenon, it was described in ways familiar at the time, as related by Brown (1989):

Nathan Wheeler saw the meteorite, a "globe of fire," as he stood outside his house in Weston early Monday morning: "its appearance was distinct and well defined, like that of the sun seen through the mist." Judge Wheeler must have been a militia man or a veteran, because he drew his precise and descriptive analogies from the drill or battlefield. The flight lasted about thirty seconds and was followed, after a short interval, by three "loud and distinct reports, like those of a four pounder, near at hand." These were succeeded by a noise similar to "a volley of musketry, protracted into what is called, in military language, a running fire," which continued for a short while after the object was lost to sight.


Benjamin Silliman and James Kingsley went to Weston on December 18 and remained for two days, interviewing witnesses, collecting specimens, and inspecting the points of impact, essentially inventing the field study of meteoritics. But right away they ran into the also newly created economic aspect of meteorites as Brown (1989) describes:

Fragments of the exploding stone had rained about the town, and one large piece struck not two rods distant from the Prince house. This intrepid family, upon discovering the treasure that had buried itself in their front yard, promptly dug it up and smashed it apart, discerning, with a sense of true Yankee economy, that if one stone could be valuable, many were more so. Others combed the countryside, searching for the telltale signs of violent impact.

Merchant Isaac Bronson...wrote on December 31 to report that an additional portion of the meteor, weighing approximately thirty-seven pounds, had been discovered near Taskaway Hill but that the discoverer had extravagant notions of its worth. Bronson offered farmer Jennings $5.00 and promised that, should he be able to obtain it at that price, Silliman might "rest assured" that it would be sent to "enrich…the curious and valuable" collection at Yale.


About 300 pounds of fragments were obtained by Silliman and Kingsley and they are the first catalogued objects in the Yale meteorite collection, which is the oldest in the US.

Silliman’s first description appeared in the Connecticut Herald on December 29. But where to publish the real scientific results became a controversial topic as there were few, well received American outlets for scientific findings at the time. An early release in France was enthusiastically received. Brown (1898) summarizes the eventual outcome, not always positive in America:

The Weston meteor drew considerable attention from across the country, even during the Embargo winter of 1807-1808. The Silliman and Day accounts appeared, in their most substantial and polished forms, in the Memoirs of the Connecticut Academy of Arts and Science nearly three years after the event, but in the intervening time the essays were published "in many newspapers, and in several literary and philosophical Journals," and always in conjunction with some mention of Yale. Thomas Jefferson is supposed to have remarked upon learning of the Yalensian theory that "it is easier to believe that two Yankee professors could lie than to admit that stones could fall from heaven.” And in the first version of Washington Irving's A History of New York (1809), narrator Diedrich Knickerbocker remarks of New England that "the people at large show a keenness, a cleverness and a profundity of wisdom that savors strongly of witchcraft—and it has been remarked that whenever any stones fall from the moon, the greater part of them is sure to tumble into New England.”


By 1818, Silliman had established the American Journal of Science largely to rectify this situation.

King and Petruny (2008) have identified 4 of the 6 reported impact sites found in contemporary news reports, with an unconfirmed anecdote of a 5th site. None are currently in Weston because the original town was subdivided after 1807, they now reside in Easton, Trumbull and Fairfield.

The primary site, the Prince house, now in Easton, is about 500 m north of a road intersection at the historic 1715 Burton House. Today this is a heavily wooded, upscale housing subdivision with a vigilant neighborhood watch.

Another potential site is located a few tens of meters west of Sturbridge Lane behind several homes within Trumbull, a very stony area.

A single large fragment was found at "the foot of Tashua Hill", also now in Trumbull, the exact location uncertain, with high ground now known as Tashua Knolls including a town recreation area surrounded by woods, homes, and shopping areas.

Reportedly a small crater ~1.5 m wide and ~1 m deep with soil and bedrock ejected up to ~50 m away formed on the farm of Elijah Seeley, who lived on Hoyden Hill. It may be the same place as the Hoyden Hills within Fairfield.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


15 valid minerals.

Meteorite/Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

Albite
Formula: Na(AlSi3O8)
Augite
Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6
Augite var. Fassaite
Formula: (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6]
Chromite
Formula: Fe2+Cr3+2O4
Diopside
Formula: CaMgSi2O6
Enstatite
Formula: Mg2Si2O6
Description: Enstatite (sensu stricto) — [En 91.5] within xenolith, Wagner et al.,1979
Enstatite var. Bronzite
Formula: (Mg,Fe2+)2[SiO3]2
'Fayalite-Forsterite Series'
Forsterite
Formula: Mg2SiO4
Ilmenite
Formula: Fe2+TiO3
Magnetite
Formula: Fe2+Fe3+2O4
Native Copper
Formula: Cu
Native Iron
Formula: Fe
Native Iron var. Kamacite
Formula: (Fe,Ni)
Nepheline ?
Formula: Na3K(Al4Si4O16)
'Orthopyroxene Subgroup'
'Plessite'
Taenite
Formula: (Ni,Fe)
Tetrataenite
Formula: FeNi
Tridymite ?
Formula: SiO2
Troilite
Formula: FeS

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Copper1.AA.05Cu
Native Iron1.AE.05Fe
var. Kamacite1.AE.05(Fe,Ni)
Taenite1.AE.10(Ni,Fe)
Tetrataenite1.AE.10FeNi
Group 2 - Sulphides and Sulfosalts
Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
Chromite4.BB.05Fe2+Cr3+2O4
Magnetite4.BB.05Fe2+Fe3+2O4
Ilmenite4.CB.05Fe2+TiO3
Tridymite ?4.DA.10SiO2
Group 9 - Silicates
Forsterite9.AC.05Mg2SiO4
Enstatite9.DA.05Mg2Si2O6
var. Bronzite9.DA.05(Mg,Fe2+)2[SiO3]2
Augite9.DA.15(CaxMgyFez)(Mgy1Fez1)Si2O6
Diopside9.DA.15CaMgSi2O6
Augite
var. Fassaite
9.DA.15(Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6]
Nepheline ?9.FA.05Na3K(Al4Si4O16)
Albite9.FA.35Na(AlSi3O8)
Unclassified
'Fayalite-Forsterite Series'-
'Plessite'-
'Orthopyroxene Subgroup'-

List of minerals for each chemical element

OOxygen
O AlbiteNa(AlSi3O8)
O Augite(CaxMgyFez)(Mgy1Fez1)Si2O6
O ChromiteFe2+Cr23+O4
O DiopsideCaMgSi2O6
O EnstatiteMg2Si2O6
O ForsteriteMg2SiO4
O IlmeniteFe2+TiO3
O MagnetiteFe2+Fe23+O4
O NephelineNa3K(Al4Si4O16)
O TridymiteSiO2
O Enstatite var. Bronzite(Mg,Fe2+)2[SiO3]2
O Fayalite-Forsterite Series
O Augite var. Fassaite(Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6]
NaSodium
Na AlbiteNa(AlSi3O8)
Na NephelineNa3K(Al4Si4O16)
Na Augite var. Fassaite(Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6]
MgMagnesium
Mg Augite(CaxMgyFez)(Mgy1Fez1)Si2O6
Mg DiopsideCaMgSi2O6
Mg EnstatiteMg2Si2O6
Mg ForsteriteMg2SiO4
Mg Enstatite var. Bronzite(Mg,Fe2+)2[SiO3]2
Mg Fayalite-Forsterite Series
Mg Augite var. Fassaite(Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6]
AlAluminium
Al AlbiteNa(AlSi3O8)
Al NephelineNa3K(Al4Si4O16)
Al Augite var. Fassaite(Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6]
SiSilicon
Si AlbiteNa(AlSi3O8)
Si Augite(CaxMgyFez)(Mgy1Fez1)Si2O6
Si DiopsideCaMgSi2O6
Si EnstatiteMg2Si2O6
Si ForsteriteMg2SiO4
Si NephelineNa3K(Al4Si4O16)
Si TridymiteSiO2
Si Enstatite var. Bronzite(Mg,Fe2+)2[SiO3]2
Si Fayalite-Forsterite Series
Si Augite var. Fassaite(Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6]
SSulfur
S TroiliteFeS
KPotassium
K NephelineNa3K(Al4Si4O16)
CaCalcium
Ca Augite(CaxMgyFez)(Mgy1Fez1)Si2O6
Ca DiopsideCaMgSi2O6
Ca Augite var. Fassaite(Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6]
TiTitanium
Ti IlmeniteFe2+TiO3
Ti Augite var. Fassaite(Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6]
CrChromium
Cr ChromiteFe2+Cr23+O4
FeIron
Fe Augite(CaxMgyFez)(Mgy1Fez1)Si2O6
Fe ChromiteFe2+Cr23+O4
Fe IlmeniteFe2+TiO3
Fe Native IronFe
Fe Native Iron var. Kamacite(Fe,Ni)
Fe MagnetiteFe2+Fe23+O4
Fe Taenite(Ni,Fe)
Fe TetrataeniteFeNi
Fe TroiliteFeS
Fe Enstatite var. Bronzite(Mg,Fe2+)2[SiO3]2
Fe Fayalite-Forsterite Series
Fe Augite var. Fassaite(Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6]
NiNickel
Ni Native Iron var. Kamacite(Fe,Ni)
Ni Taenite(Ni,Fe)
Ni TetrataeniteFeNi
CuCopper
Cu Native CopperCu

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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