Battle Mountain (Virginia)
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Battle Mountain is an
igneous Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma or ...
mountain in
Rappahannock County Rappahannock County is a county located in the northern Piedmont region of the Commonwealth of Virginia, US, adjacent to Shenandoah National Park. As of the 2020 Census, the population was 7,348. Its county seat is Washington. The name "Rappah ...
,
Virginia Virginia, officially the Commonwealth of Virginia, is a state in the Mid-Atlantic and Southeastern regions of the United States, between the Atlantic Coast and the Appalachian Mountains. The geography and climate of the Commonwealth ar ...
. The eastern slope is generally considered to reside in the unincorporated town of
Amissville, Virginia Amissville ( ) is an unincorporated community in Rappahannock County in the U.S. commonwealth of Virginia. It is located on U.S. Route 211 about halfway between Warrenton and the small town of Washington, Virginia. The Locust Grove/R.E. Luttre ...
while the western slope is generally considered to be within
Castleton, Virginia Castleton is an unincorporated community in Rappahannock County in the U.S. state of Virginia. It is located northwest of Culpeper. Culture Maestro Lorin Maazel maintained a estate in Castleton, and made it the focus of the Castleton Festi ...
. The entire mountain including the
summit A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topography, topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used ...
lies within private property at an elevation of 1,162 ft (354.2 m).


Geology


Tectonic emplacement and geochronology

It is an extinct volcano dating to the
Neoproterozoic The Neoproterozoic Era is the unit of geologic time from 1 billion to 538.8 million years ago. It is the last era of the Precambrian Supereon and the Proterozoic Eon; it is subdivided into the Tonian, Cryogenian, and Ediacaran periods. It is ...
and is approximately 704 million years old (+/- 4 million years) as dated using the U- Pb zircon crystal
geochronology Geochronology is the science of determining the age of rocks, fossils, and sediments using signatures inherent in the rocks themselves. Absolute geochronology can be accomplished through radioactive isotopes, whereas relative geochronology is pr ...
method. It is a unit of the Robertson River Igneous Suite and is located within the Blue Ridge
anticlinorium In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core, whereas a syncline is the inverse of an anticline. A typical anticline is convex up in which the hinge or crest is the l ...
. This volcanic formation was a result of crustal extensional
rifting In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben ...
of the eastern
Laurentia Laurentia or the North American Craton is a large continental craton that forms the ancient geological core of North America. Many times in its past, Laurentia has been a separate continent, as it is now in the form of North America, although ...
n margin of the
supercontinent In geology, a supercontinent is the assembly of most or all of Earth's continent, continental blocks or cratons to form a single large landmass. However, some geologists use a different definition, "a grouping of formerly dispersed continents", ...
Rodinia Rodinia (from the Russian родина, ''rodina'', meaning "motherland, birthplace") was a Mesoproterozoic and Neoproterozoic supercontinent that assembled 1.26–0.90 billion years ago and broke up 750–633 million years ago. were probably ...
. This was the beginning of a chain of events that ultimately gave birth to the precursor
Atlantic The Atlantic Ocean is the second-largest of the world's five oceans, with an area of about . It covers approximately 20% of Earth's surface and about 29% of its water surface area. It is known to separate the " Old World" of Africa, Europe an ...
, the
Iapetus Ocean The Iapetus Ocean (; ) was an ocean that existed in the late Neoproterozoic and early Paleozoic eras of the geologic timescale (between 600 and 400 million years ago). The Iapetus Ocean was situated in the southern hemisphere, between the paleoco ...
at 550 Ma during the
Ediacaran The Ediacaran Period ( ) is a geological period that spans 96 million years from the end of the Cryogenian Period 635 million years ago (Mya), to the beginning of the Cambrian Period 538.8 Mya. It marks the end of the Proterozoic Eon, and th ...
Cambrian The Cambrian Period ( ; sometimes symbolized C with bar, Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million ...
transition.


Geochemical evolution

The volcano is composed of
alkali feldspar Feldspars are a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium. The most common members of the feldspar group are the ''plagioclase'' (sodium-calcium) feldspa ...
granitic A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar. Granitoids range from plagioclase-rich tonalites to alkali-rich syenites and from quart ...
rock of the Robertson River
Igneous Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma or ...
Suite. This includes
felsic In geology, felsic is a modifier describing igneous rocks that are relatively rich in elements that form feldspar and quartz.Marshak, Stephen, 2009, ''Essentials of Geology,'' W. W. Norton & Company, 3rd ed. It is contrasted with mafic rocks, whi ...
complex material such as
biotite Biotite is a common group of phyllosilicate minerals within the mica group, with the approximate chemical formula . It is primarily a solid-solution series between the iron-endmember annite, and the magnesium-endmember phlogopite; more alumino ...
,
hornblende Hornblende is a complex inosilicate series of minerals. It is not a recognized mineral in its own right, but the name is used as a general or field term, to refer to a dark amphibole. Hornblende minerals are common in igneous and metamorphic rocks ...
-biotite,
magnetite Magnetite is a mineral and one of the main iron ores, with the chemical formula Fe2+Fe3+2O4. It is one of the oxides of iron, and is ferrimagnetic; it is attracted to a magnet and can be magnetized to become a permanent magnet itself. With the ...
, and
alkali In chemistry, an alkali (; from ar, القلوي, al-qaly, lit=ashes of the saltwort) is a basic, ionic salt of an alkali metal or an alkaline earth metal. An alkali can also be defined as a base that dissolves in water. A solution of a ...
granitic
rock Rock most often refers to: * Rock (geology), a naturally occurring solid aggregate of minerals or mineraloids * Rock music, a genre of popular music Rock or Rocks may also refer to: Places United Kingdom * Rock, Caerphilly, a location in Wales ...
including
rhyolite Rhyolite ( ) is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained groundmass. The mineral ...
on the eastern slopes of Battle Mountain and the adjacent (and geologically related) Little Battle Mountain (elevation 937 feet).


Palaeogeographic reconstruction

A unique geological feature of Battle Mountain is that the western slope outcrops are composed entirely of alkali feldspar granite, while the eastern slope up to and including the summit is entirely rhyolitic. This provides strong evidence of a theorized lateral explosive eruption event centered on the eastern slope at approximately 704 Ma as proposed by Woolman (2016). Further mathematical geology evidence which supports this theory includes a palaeogeographic reconstruction of the mountain by Woolman utilizing
artificial neural networks Artificial neural networks (ANNs), usually simply called neural networks (NNs) or neural nets, are computing systems inspired by the biological neural networks that constitute animal brains. An ANN is based on a collection of connected unit ...
and
Markov chain A Markov chain or Markov process is a stochastic model describing a sequence of possible events in which the probability of each event depends only on the state attained in the previous event. Informally, this may be thought of as, "What happe ...
geostatistical Geostatistics is a branch of statistics focusing on spatial or spatiotemporal datasets. Developed originally to predict probability distributions of ore grades for mining operations, it is currently applied in diverse disciplines including petro ...
models including period climate condition-based soil erosion rates, Kirkby's hillslope movement evolution equations and recursive biogeochemical soil erosion rates in felsic granitic conditions. The result was the digital reconstruction image shown on the left, indicating what Battle Mountain may have looked like 704 million years ago on the western slope.


Only known volcanic mountains in Rappahannock County, VA

Battle Mountain and Little Battle Mountain are the only mountains in Rappahannock County which are known to be
volcanic A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates a ...
in origin, and are among the oldest visibly intact extinct volcanoes in Virginia. White
quartz Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical form ...
boulders In geology, a boulder (or rarely bowlder) is a rock fragment with size greater than in diameter. Smaller pieces are called cobbles and pebbles. While a boulder may be small enough to move or roll manually, others are extremely massive. In co ...
and smaller fragments are common on and around Battle Mountain, a result of molten
silica Silicon dioxide, also known as silica, is an oxide of silicon with the chemical formula , most commonly found in nature as quartz and in various living organisms. In many parts of the world, silica is the major constituent of sand. Silica is one ...
that was contained in the rhyolite
lava Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or un ...
and granitic
magma Magma () is the molten or semi-molten natural material from which all igneous rocks are formed. Magma is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natural sa ...
that formed the volcano. As quartz is extremely
hard Hard may refer to: * Hardness, resistance of physical materials to deformation or fracture * Hard water, water with high mineral content Arts and entertainment * ''Hard'' (TV series), a French TV series * Hard (band), a Hungarian hard rock supe ...
relative to feldspar granite and rhyolite, it tends to remain present on the surface while the softer granite it was embedded in wears away into the soil.


Access

The nearest unincorporated town is
Amissville, Virginia Amissville ( ) is an unincorporated community in Rappahannock County in the U.S. commonwealth of Virginia. It is located on U.S. Route 211 about halfway between Warrenton and the small town of Washington, Virginia. The Locust Grove/R.E. Luttre ...
at approximately 4 miles away. Access to the mountain and the summit must be negotiated with local
landowners In common law systems, land tenure, from the French verb "tenir" means "to hold", is the legal regime in which land owned by an individual is possessed by someone else who is said to "hold" the land, based on an agreement between both individual ...
first as the mountain, including all portions of the July 1863 battlefield exists entirely on private property.


Agriculture

The various slopes of Battle Mountain are in either commercial timber (primarily mixed hardwoods), cattle pasture (western slope) or crops (corn, hay and pumpkins as of 2019). Battle Mountain Farm, which comprises the majority of the eastern slope of Battle Mountain is a mixed hardwood timber and small-scale commercial pumpkin grower, specializing in large jack-o-lantern pumpkins. Their pumpkins are grown without herbicides or pesticides in multiple commercial-scale 60-foot by 5-foot ecologically sustainable raised beds (no soil tilling required) using locally produced natural fertilizers. The beds also utilize water-conserving polymer mulch and irrigation drip lines attached to on-site wells approximately 300 feet deep, providing mineral-rich water from volcanic aquifers. The well water pressure is provided by a 10.4 kilowatt grid-tied solar panel array on the farm, with lead-acid battery backup.


References

{{Mountains of Virginia Mountains of Virginia Blue Ridge Mountains Rappahannock County, Virginia Volcanoes of Virginia Stratovolcanoes of the United States