Drunk on Paleontology - Madonna Estate Dolcetto

 

The next Drunk on Geology is for the Madonna Estate Dolcetto by the Madonna Estate Winery from Napa, California. 

This Drunk on Geology is a little different because the geological nature of the wine is not in the name, or the label, but in the logo of the Madonna Estate Winery itself. 

The logo, as seen here a little better, is what is known as Fermat's spiral. 

Fermat's Spiral. Image courtesy of MSU.edu.

Here are a couple of clearer shots of the logo. 

On the front of the bottle.

And on the bottle cork cover. 

Now the reason that I am enamored with the logo, is that this is the same design that my favorite trace fossil, Spirorhaphe, makes. A trace fossil is a fossil that is left behind by the behavior of an organism, like a footprint or a worm burrow, but not a fossil of the actual organism itself. Trace fossils are also named based on their morphology, similar to animals. Spirorhaphe, in particular, is a trace fossil that is part of a group of trace fossils known as graphoglyptids. These fossils form as open burrows, often in deep water at the bottom of the ocean. 

Graphic of graphoglytid preservation. Image courtesy of my dissertation.

These open burrow systems often have intricate patterns to them. They are preserved when a turbidite, which is essentially an underwater landslide, comes down on top of where the graphoglytid burrows are located. The turbidite churns up the water and removes the top layer of sediment over the burrow. The turbidite then deposits the sand and mud that was transported on top of the bottom half of the open burrows creating a cast of the burrows, preserving the intricate burrow system.

Images of some common graphoglyptids. A) Cosmorhaphe. B) Helminthorhaphe. C) Megagrapton. D) Paleodictyon. E) Spirorhaphe. F) Urohelminthoida. 

Above is an example of some of the varied shapes that come from this group. Scientists aren't sure what the animals that lived in the burrows were doing but the thoughts range from filtering their food out of the sediment, to growing bacteria on the walls to eat, to trapping organisms within the burrow walls and eating those. The one that interests me the most in this instance is Spirorhaphe, which has the same design as the logo!

Example of Spirorhaphe from the Late Cretaceous of Tanzania. 

Initially named in 1895 by Fuchs, Spirorhaphe is an ichnogenus (a genus of a trace fossil) that has gone through a rather tortuous history with many ichnospecies (a species of a trace fossil) being attributed to it and then those definitions changing. Currently, there are three species associated with Spirorhaphe, however even those are contentious in the scientific community. 

Regardless, Spirorhaphe is a fantastic trace fossil and my favorite to boot. 

Text on the back of the bottle:

"Like the cave drawings of Lascaux, Madonna Estate's label represents a history of generations - four generations - that have grown grapes and produced varietal wines with rich concentrated flavors. The continuity of our spiral symbolizes an ongoing commitment to create fine wines."

Drunk on Mineralogy - Lucky Rock Pinot Noir

 

The next Drunk on Geology is for Lucky Rock Pinot Noir from the Lucky Rock Wine Co.

A "Lucky Rock" is gold or a rock containing gold, as mentioned on the Lucky Rock Wine Co.'s website. The chemical symbol for gold is Au, and gold is one of the unique minerals that, in its pure form, is composed entirely of one element. It has a hardness of 2.5 to 3 on the Mohs hardness scale meaning that it actually is very soft (your fingernail is 2.5). For this reason most gold jewelry is mixed with another metal to prevent scratching and bending easily. The karat rating of the gold represents it's purity, where 24 karat is 99.9% pure, 22 karat 91.7%, 18 karat 75%, and so on. Gold naturally does not corrode or tarnish, so even when it is mixed with other metals it usually has a resistance to tarnishing, enhancing its value for jewelry. When gold is found in place, the highest grade of gold is often found in association with quartz veins. Currently gold is considered one of the most valuable metals on Earth, being used as the standard for most money (gold standard).

Lucky Rock logo description from the Luck Rock Wine Co Website.

Gold is often formed initially in relation to volcanic regions, where fluids associated with volcanoes carry the heavy metals up towards the surface and deposit them in rocks. These are found in areas of current or former subduction zones, places where two plates came together forcing one place down and melting it, while the other plate is forced upwards into mountains. Afterwards, erosion will take the gold out of the mountains and carry them down stream. However, since gold is so dense it does not travel easily down rivers and will often settle to the bottom of the river within the rocks and mud within the river sediment. These gold deposits are known as placer deposits and are the primary place where gold panners find gold. They can then use the locations of these placer deposits to backtrack to the original sources of the gold within the streams.

The website also mentions that "Lucky Rock Wine Co., (is) named after one of the more memorable mines they grew up at." So I decided to send them a message to see if I could find out a little more information. This is what one of the owners of Lucky Rock sent back:

"My dad started prospecting and mining in the early 80's in Siskiyou County. He and a partner filed claims for two mines in the Klamath National Forest around 1984 - the hard rock mine was called Lucky Rock. In addition, my dad and a partner sourced funding for their mining efforts and eventually had several investors from Southern California. The company was named Lucky Rock Mining Company and operated for a few years. The "Lucky Rock" mine was just outside Seiad Valley."

Text from the back of the bottle:

"We grew up in a mining family, digging through the soil for a "Lucky Rock." Now our search has turned to discovering California's lucky vineyards from which we craft this tasty Pinot Noir."

With this information I was easily able to find the Lucky Rock mining claims.

Lucky Rock Mining Co mining claims. Map and information from The Diggings.

And as usual, let's take a look at the geologic map of that region, just to get a handle of what we are looking at.

Geologic map of the Seiad Valley region. Map courtesy of the NGMDB. 

The dominant geological features of this region are by far the Slinkard Pluton, identified as unit Mzd, and the blue unit listed as MzPz towards the north of that. On that specific map Mzd is identified as Dioritic Plutonic rocks and MzPz is some Mesozoic and Paleozoic undifferentiated metamorphoric basement rocks. The Slinkard Pluton however is the major producer of the gold identified within the region. A pluton is a igneous body that formed from the cooling of a body of magma below the Earth's surface. 

Diagram of a subduction zone. Image courtesy of the NPS.

Off the west coast of northern California, as well as Oregon and Washington, is what is known as a subduction zone. In a subduction zone one plate goes beneath the other. As the one plate sinks down, it starts to heat up and melt. That melted plate then rises up and forms a line of volcanoes.

Plates along the northwestern coast of North America. Image courtesy of the NPS.

Along the western edge of northern California is the subduction of the Gorda Plate, which is the remnant of the much larger Farallon Plate that used to be subduction along the entire Californian coast. 162 million years ago, during the Late Jurassic, the melted portions of the Gorda Plate produced the Slinkard Pluton as well as the related Wooley Creek batholith (which is a much larger pluton). 

As the magma body was cooling, the heat from the magma also heated up the surrounding groundwater. This groundwater, as it was heated rose to the surface, cooled, and descended back down to the magma body, creating a cycle. As the hydrothermal fluids moved from the magma towards the surface and through the surrounding rocks, they moved the heavy metals (such as gold, copper, silver, etc.) from within the magma and redeposit them within the surrounding landscape. Over time the gold would weather out of the surrounding landscape and get transported within neighboring streams and rivers. But due to the density of gold, it would often sit at the bottom of streams until a strong enough current came along to move it further along. These deposits, known as placer deposits, are what the Lucky Rock Mining Co. was searching for.

Drunk on Petrology - Rockpile Zinfandel

 

The next Drunk on Geology is for Rockpile Zinfandel from Mauritson Wines. 

The name of Rockpile is the same as the region in which the vineyards are located. The Rockpile region was a recent AVA denoted in 2002. According to the TTB, an AVA is an American Viticultural Area which is:

"delimited grape-growing region with specific geographic or climatic features that distinguish it from the surrounding regions and affect how grapes are grown."

The specifics of the Rockpile AVA are that it is the northern extent of the Dry Creek Valley AVA that encompasses the areas from 800 to 2,000 feet in elevation with steep, rocky slopes and rocky loam/ clay-loam soils. 

Looking at the geology of the region, most of the Rockpile AVA falls within one specific geological unit. 

Geological map of the Rockpile AVA. Map obtained from the NGMDB. 

The Rockpile AVA runs along the southwestern shores of Lake Sonoma towards the north. This region is all encompassed by the KJfs formation on the geological map above. The KJfs is the Jurassic to Cretaceous age Franciscan Complex, specifically the greywacke and mélange deposits. The Franciscan Complex is a series of rocks that are termed accretionary (or accreted) terrain. These accreted terrains were added onto North America due to the subduction zone that used to lie on the western shore of California.

Diagram of the subduction zone that was formerly off the western California coast. Image courtesy of the NPS. 

Starting around 100 million years ago, the Farallon Plate started subducting beneath the North American Plate. As that happened, the islands and other land masses that were on the Farallon plate were scraped off and stuck onto the North American plate in a region known as the accretionary wedge. The Franciscan Complex is such an accretionary wedge that was built up from oceanic crust and pelagic deposits over the course of the Jurassic and Cretaceous. Over time the subduction zone was subducted as well beneath North America, with the remaining parts of the subduction zone only occurring currently along the western coast of Washington, Oregon, and the very northern part of California. 

Extent of the Franciscan Complex in California. Image courtesy of Raymond, 2019.

The rocks within this complex are a large mishmash of materials all thrown together due to the way they accumulated on the continent. As mentioned above, the primary rocks within the Rockpile region are denoted as greywacke and mélange. Greywacke is kind of a bucket term, which is sometimes used for a poorly sorted, grey sandstone. However the Dictionary of Geological Terms 3rd Ed. identifies greywacke (AKA graywacke) as:

"An old term, now generally applied to a dark gray firmly indurated coarse-grained sandstone that consists of poorly sorted angular to subangular grains of quartz and feldspar, with a variety of dark rock and mineral fragments, embedded in a compact clayey matrix having the general composition of slate and containing an abundance of very fine-grained illite, sericite, and chloritic minerals. Graywacke commonly exhibits graded bedding and is believed to have been deposited by submarine turbidity currents.  

The submarine deposition of these rocks makes sense, since they were likely formed along the sea floor before they were scraped off by North America. A turbidity current is an underwater landslide.

On the other hand, the term mélange just typically means a mixture rock blocks of varied sizes and lithologies, not in contact with each other, and surrounded by a finer-grained matrix. Typically these are formed by the process of amalgamation within the accretionary wedge. 

 

Text from the back of the bottle:

"In 1868 our family established a homestead in the Rockpile area of Northern Sonoma County. The first vines were planted in 1884, starting a tradition of farming that has spanned six generations. Today we craft small production, single vineyard wines that showcase the diversity of Rockpile's rugged terrain. From our vineyards to your glass we thank toy for sharing this tradition" - The Mauritson Family

 

According to the USGS:

"The sedimentary model suggests that blocks (olistoliths) were transported into the depositional environment of the matrix material by gravity driven debris slides.  The trench associated with the subduction zone provides an area of suitably steep slope for this theory and the converging plates bring the displaced terranes into proximity of the continental margin mélange matrix.  The resulting olistostrome then underwent the deformation described above, disrupting the original depositional character of the matrix/block relationships.  The tectonic model suggests that primary incorporation of blocks into mélange was by tectonic processes.  During and after accretion, lenses of rock derived from incoming exotic terranes were interleaved with continental margin deposits by faulting.  Subsequent deformation during uplift further broke up the lenses of exotic rocks, forming the mélange blocks observed today."

So in summary, the rocks within the Rockpile AVA were formed from submarine landslides that eventually got scraped off the sea floor and jumbled together within the western edge of the North American continent.

References
https://www.mauritsonwines.com/Wines/Rockpile-Wines
https://www.sanfranciscowinetours.com/appellations/rockpile.php
https://www.ttb.gov/wine/american-viticultural-area-ava 
https://www.nps.gov/subjects/geology/plate-tectonics-subduction-zones.htm 

https://ngmdb.usgs.gov/mapview/?center=-123.038,38.74&zoom=12

https://www.mdpi.com/2076-3263/9/8/338/htm

https://pubs.usgs.gov/mf/2002/2402/mf2402ada.txt

https://link.springer.com/referenceworkentry/10.1007%2F3-540-31079-7_135

Drunk on Petrology - Bedrock Old Vine Zinfandel

 

The next Drunk on Geology is for Bedrock Old Vine Zinfandel by the Bedrock Wine Company. 

Although I am pretty certain that the owners of the winery chose to use the term "bedrock", with the less geological definition of the word as the foundation of their winery, that is not the way a geologist would see it. And I see it, as a geologist would see it. Bedrock Wine Company also has a large number of vineyards, however only one bear's the name "Bedrock" so we are going to focus on that one.

Bedrock definition (courtesy of the Dictionary of Geological Terms 3rd Ed.):

The solid rock that underlies gravel, soil, or other superficial material.

The problem with determining the bedrock of a region, especially an area within a river valley, such as where the Bedrock Vineyards are located, is that the overlying gravel, soil, and other superficial materials are frequently what is published on geological maps. And that is the case here, so we need to infer what indeed is the bedrock beneath the superficial materials. There are sometimes geologic bedrock maps made which interpret what would be the bedrock below the superficial deposits, however I couldn't find one for this region. This map is also a fairly recent map (2017), so I am fairly confident that we can use it to determine the likely bedrock below the sediment. 

Geological Map of the Bedrock Vineyards locality. Map courtesy of the NGMDB. 

The red circle on the map above denotes the area of the Bedrock vineyards. As you can see there is a lot of geologic deposits where the only capital letter is a "Q". The "Q" stands for the Quaternary, the time period they were deposited during and these are the superficial deposits as mentioned above. The Quaternary represents the last ~2.5 million years in the Earth's geological history and runs up to today. These are mostly sediment deposited by the Sonoma Creek that runs down the middle of the valley. 

In order to determine the bedrock from a map like this we need to first look at the bedrock along the outside edges of the stream valley deposits. These are going to be the sediments that begin with capitol letters besides just "Q". You can determine what all of these abbreviations by looking at the original map and legend HERE.

Text from the back of the bottle:

"From vines averaging over 80 years in age planted throughout the diverse state of California, this wine aims to reflect the perfume, freshness, and spice that makes Zinfandel so utterly delicious. Fermented with native yeasts and minimally racked, this wine should provide great short-term drinking but will age gracefully for 5-10 years."

The most notable rock formations are QPge, PMpu, Msvrah, and Msvas. Since QPge spans both sides of the river sediments, I am inclined to believe that this is the most likely bedrock directly below the winery. Even though I said that the deposits starting with a "Q" represented overlying sediment, there is also a capitol "P" on these. The "P" indicates that the unit spans more than just the Quaternary. 

The QPge represents the Glen Ellen Formation. The Glen Ellen Formation is a unit comprised of a mixture of tuffaceous clay, mud, bouldery to pebbly gravel, and sand and silt deposits with interbedded conglomerates. These sediments were deposited in a variety of nonmarine environments, including coalescing alluvial fans, fan deltas, streams, and lakes (per Sweetkind et al., 2010). The Glen Ellen formation is Pliocene to Pleistocene in age and is identified as younger than 3.2 million years old. These rocks were likely deposited in a prehistoric version of the Sonoma Creek in which is currently found in the valley now. 

The PMpu is the Pliocene-Miocene age Upper Petaluma Formation. The Petaluma Formation is dominated by deposits of moderately to weakly consolidated silty to clayey mudstone, with local beds and lenses of poorly sorted sandstone. The environment in which these rocks were deposited consists of transitional marine and nonmarine sediments that were deposited in estuarine, lacustrine, and fluvial depositional settings (per Sweetkind et al., 2010). These rocks represent a much higher sea level than the Glen Ellen Formation, with a mixture of marine and nonmarine rocks deposited within the valley. 

Msvrah (?Rhyolite of Adobe Canyon) and Msvas (Andesite of Shocken Hill) are both a part of the Sonoma Volcanics. The Sonoma Volcanics were deposited across a long range of time from the Miocene through the Pliocene and are described by the USGS as:

"... a thick and highly variable series of continental volcanic rocks, including andesite, basalt, and minor rhyolite flows and interbedded coarse- to fine-grained pyroclastic tuff and breccia, redeposited tuff and pumice, and diatomaceous mud, silt, and sand."

So overall, it is likely the bedrock for the Bedrock Vineyard is the Glen Ellen Formation, however the Upper Petaluma Formation is also likely. These are likely sprinkled with local volcanic deposits from the Sonoma Volcanics as well. 

References
https://ngmdb.usgs.gov/mapview/?center=-122.503,38.3&zoom=14
https://ngmdb.usgs.gov/Prodesc/proddesc_105819.htm
https://pubs.geoscienceworld.org/gsa/geosphere/article/6/3/237/132359

https://pubs.usgs.gov/wsp/1495/report.pdf

Drunk on Petrology - Chalk Hill Syrah

 

The next Drunk on Geology is for Chalk Hill Syrah from the Chalk Hill Estate Winery. 

The name of the Chalk Hill Estate Winery comes from Chalk Hill upon which it sits, but the winery encompasses a rather large area with several different types of soil and bedrock. From their own website:

"In amazing proximity, the soils range from shallow to deep, from thin to thick, from gravel and rock to heavy clay. An old river bed caps one hill; an unusual serpentine vein ranges through another and, under the topsoil, is a distinctive layer of chalk-colored volcanic ash which inspired the name of Chalk Hill, the appellation, and the estate."

Their description of the winery is geologically fantastic, so lets take a closer look at the actual geologic map of the region. 

 

The winery is located within the red circle on the geologic map above. This region, and the surrounding area, is a mishmash of geology. Starting with the purple unit that crosses the middle of the red circle, we have the serpentine vein that is mentioned in the description.  

Geologic Map of the Chalk Hill Winery region. Map located using the NGMDB. 

Although identified by the winery as "unusual", the serpentine band is actually part of a Middle Jurassic formation known as an ophiolite, of which ophiolites are fairly common across California. This is because of how California formed. The diagram below illustrates the subduction zone that was formerly off the western coast of California. 

Diagram of the subduction zone that was formerly off the western California coast. Image courtesy of the NPS. 

The crust of the Earth is made up of plates that move around and a subduction zone is when one plate goes beneath the another plate. When that occurs, a lot of things happen. As the plate descends, it starts to melt. That melted rock then rises back up producing volcanoes, in this instance it is how the Sierra Nevada mountains formed. But as that plate is descending, the overriding plate (in this instance North America) is scraping the top layer of the down-going plate (the Farallon Plate). The scraped material includes any islands in the ocean, other land masses, and even pieces of oceanic crust. This material is known collectively as "accreted terrane", and is how a vast portion of California was built up over time.  

Looking at the pieces of the oceanic crust in particular, as the oceanic crust is formed, it is created at the Mid Ocean Ridge (as seen on the diagram above), by a series of continuous volcanic eruptions. These volcanic eruptions produce layers of different rocks and minerals depending on how the eruption interacts with the other rocks and water in the area. This eventually creates a layer-cake of rocks that are known as an Ophiolite Sequence.

Idealized ophiolite sequence. Image courtesy of Arenas et al., 2007.

One of the lowermost levels of an ophiolite sequence is the Serpentinite layer. The serpentinite is formed from the hydrothermal (hot water) metamorphism of mantle rocks, producing these green mineral rich rocks (most frequently comprised of antigorite, lizardite, and chrysotile) with a surface that looks similar to snake skin (hence the name). 

One of the other main rock formations in the region of the winery is the KJgvs, which is part of the Jurassic-Cretaceous Great Valley complex. This particular series of rocks consists of interbedded sandstone, siltstone, and shale formed within the Great Valley forearc basin as seen in the subduction zone diagram above. These are non-marine rocks including river complexes across the valley. 

Most of the rocks within this region, however, are part of the Sonoma Volcanics,  including the Tsb rock, which is a basalt. According to the USGS:

The Sonoma volcanics constitute a thick and highly variable series of continental volcanic rocks, including andesite, basalt, and minor rhyolite flows and interbedded coarse- to fine-grained pyroclastic tuff and breccia, redeposited tuff and pumice, and diatomaceous mud, silt, and sand. A prominent body of rhyolite flows and tuff with some obsidian and perlitic glass called the St. Helena rhyolite member, occurs in the upper part.

The final location we will talk about would the the eponymous Chalk Hill. Chalk Hill is to the east of the winery with the winery sitting near its base along the Chalk Hill road (as near as I can tell). And as the Chalk Hill Winery website describes, Chalk Hill is indeed not made up of chalk. Chalk is a well known sedimentary rock, most famously found as the White Cliffs of Dover. Chalk itself is made up of tiny fossils of animals called coccolithophores. The microscopic animals form a ball covered in little calcium carbonate plates called coccoliths. When the animal dies, the plates come apart and if enough of the animals are present in the environment, they can accumulated over time to form the rock known as chalk, which is a white to grey colored chalky rock.

However, that is not what we have here. We have a rock that resembles the color and texture of chalk, but is not actual chalk. This rock is made up of ash and other pyroclastic deposits from the nearby volcanic zones produced from the subduction zone that continued off to the west. Ash, also a white to grey chalky rock, has a strong resemblance to chalk, hence the name of the region and the hill. When ash falls, it quickly hardens and produces a rock layer known as tuff. Although the term tuff can refer to any pyroclastic (volcano produced) rocks. The tuff of Chalk Hill was deposited mostly within water bodies in the region as part of the Sonoma Volcanics. These ash deposits have been dated to ~4 to 5 million years ago. 

References
Arenas, Ricardo & Catalán, J.R. & Martínez, Sonia & García, Florentino & Abati, Jacobo & Fernández-Suárez, J. & Andonaegui, P. & Gómez Barreiro, Juan. (2007). Paleozoic ophiolites in the Variscan suture of Galicia (northwest Spain): Distribution, characteristics and meaning. 10.1130/2007.1200(22). 
https://pubs.usgs.gov/wsp/1495/report.pdf
https://www.nps.gov/subjects/geology/plate-tectonics-subduction-zones.htm

https://ngmdb.usgs.gov/Prodesc/proddesc_52762.htm

https://pubs.geoscienceworld.org/gsa/geosphere/article/8/2/342/132533/Evolution-of-the-Rodgers-Creek-Maacama-right

Drunk on Petrology - Soda Rock's Lord Snort Blanc

 

My next Drunk on Geology post is for Soda Rock's Lord Snort Blanc from the Soda Rock Winery. 

The winery was named "Soda Rock" back in in the 1930's following the repeal of prohibition, a name that has been passed down through several different owners. The original name of the winery descended from the Soda Rock Post Office and General Store, a building which the winery took over after it had fallen into disrepair. The name of Soda Rock appears to be named after an outcrop of rock along the nearby Russian River, identified on topographic maps simply as "Soda Rock". 

Soda Rock feature on the topo maps. Image from the NGNDB.

Since the actual Soda Rock lies within the Russian River it is a bit difficult to identify which specific geologic formation it belongs to. However we can look at the nearby geological formations and see what fits best. The closest, and most likely, is the Pleistocene and Pliocene age (~5-2 million years old) Glen Ellen Formation (QTge on the map below). The Glen Ellen Formation is identified as "compact lenticular poorly sorted silly clay, sand, poorly cemented conglomerate, and local fairly loose sand and gravel. There is also a tuffaceous member of the Glen Ellen Formation within the region, although not mapped right in this area.

Soda Rock feature on the geological maps. Image from the NGNDB.

The other potential rock near that area are the slightly more pinkish rocks on the map above. These are Pliocene and Miocene age (~20-5 million years old) Sonoma Volcanics (Tsb on the geologic map). Which are mainly andesite and basalt lava flows, pyroclastic rocks, and mud flows with interbedded volcanic sediments. Thick sections of poorly permeable tuff breccia and rubbly and fractured zones in lava yield water to wells. 

Soda Rock from Google Street View. 

Based on the view from Google Earth, which luckily had a "street view" along the Russian River, we can get a fairly good view of the Soda Rock itself. Unfortunately, this is no substitute for going out and viewing the rock in person. So any guess as to what the rock actually is, is entirely a guess on my part, but this looks to me more like a volcanic deposit. This means that the Soda Rock itself is more likely to be part of the Sonoma Volcanics, than a sedimentary deposit, which would be part of the Glen Ellen Formation.

The term "soda" is also a geological term, although one that is not often used in scientific circles (from what I am familiar with). It seems to be a more commercial/industrial term and it refers to sodium, specifically sodium carbonate (Na2CO3). Sodium within rocks also has a tendency to produce a grey, ashy looking rock, of which the term "soda ash" is also another commercial term for the word "soda". So, regardless of geology, the Soda Rock in the river, does appear to have a grey, ashy look to it, hence rendering it understandable that one would call it "soda". 

Text from the bottle:

"Located in the heart of the renowned Alexander Valley in Northern Sonoma County, Soda Rock Winery's rich heritage dates back to 1869 when the winery site housed the Soda Rock Post Office and General Store.

Today Soda Rock Winery's Village Heritage continues as owners Ken and Diane Wilson bring new life to this historic site with the best that Alexander Valley has to offer."

As a side note, I picked the Lord Snort Blanc as the wine for this post because the whole reason we stopped at this winery was the fantastic pig sculpture just outside the main wine tasting building, dubbed Lord Snort. A sculpture by artist Bryan Tedrick that is 20,000 pounds steel statue measuring 32 ft wide, and 20 ft tall. Lord Snort made his debut at the Burning Man Festival and eventually found his way to the winery.

 

And of course we had to take our picture in front of Lord Snort with our Lod Snort Blanc.