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    Each of the pictured bottles has a relatively short description and explanation including estimated dates or date ranges for that type bottle and links to other view pictures of the bottle.

    Additional links to images of similar bottles are also frequently included.

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    The array of references used to support the conclusions and estimates found here - including the listed completely dating site g ranges completely dating site g are noted. Additional information completely dating site g estimates are based on the empirical observations of the author over 50 years of experience; this is often but not always noted.

    Various terminology is used in the descriptions that may be unfamiliar if you have not studied other pages on this site.

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    If a term is unfamiliar, first check the Bottle Glossary page for an explanation or definition. As an alternative, one can do a search of this website. Figured Flasks Figured flasks is a generic name for the large class of liquor flasks primarily produced between and Due to their esthetic and decorative nature, these flasks were infrequently discarded unless broken so many survived to the present day. Figured flasks also include c alabash bottles example belowwhich are covered separately here because of their distinctive shape, and some flasks that fit the form description but are just embossed with lettering, i.

    Unlike most other types of liquor bottles which are generally more common without embossing, figured flasks are by definition embossed since the embossed motifs and molded designs are what defines them as figured flasks, though many shapes are also unique to this group e. Unembossed flasks with shapes similar to some of the later s primarily figured flasks are considered generically in the "Flask not considered figured " category.

    The figured flasks described here represent a small cross-section of the hundreds of different types made during their heyday. These type items are occasionally found on historic archaeological sites though usually as fragments since they were not usually discarded until broken. This book is the source of information on figured flasks and contains by far the most comprehensive listing with illustrations and is the accepted classification system for figured flasks.

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    Here the authors divide figured flasks into completely dating site g distinct "Form Groups" and includes dating ranges for when that form group was first produced. The book also covers most other types of 18th and 19th century American bottles and is an almost mandatory reference for serious students of American made bottles of the 18th and 19th century.

    Because of the beauty - and possibly the intrinsic value - of figured flasks, many have been reproduced at various times during the 20th century. Some of these reproductions are very hard to discern from originals to the inexperienced eye. The bottles pictured in this section are all early to midth century originals. Decorative flasks The decorative group of flasks is a category of "pictorial" flasks made up of four primary types: The figured flask pictured to the left and the colorful group of five to the upper right is commonly referred to by collectors as a scroll flask, though in the early days of collecting and probably even now they were referred to as "violin" flasks.

    What 19th century glass makers called these is lost to history. This style of flask was introduced around and were extremely popular through the s and s. Popularity apparently waned by the beginning of the Civil War early s and it appears that very few if any were made after that time.

    Most scroll flasks were likely made by Midwestern glassmakers, though most do not have makers marks to allow for precise attribution. Scroll flasks were primarily made in half-pint, pint most common size by farand quart sizes, though smaller and larger examples are known, including a gallon size. Scroll flasks almost always have some type of pontil scar, i.

    The range of colors possible in these flasks is almost unlimited, though they were by most commonly made in shades of aquamarine - like the example above.

    Finishes found on these flasks included primarily the following: The aqua scroll flask pictured above is very typical in design and likely dates from the late s or s. Click on the following links for more images of this pint scroll flask from different views: To the right is pictured a very similar pint scroll flask GIX in an unusual yellow green color with a cracked-off and non-refired finish; click thumbnail image to enlarge.

    Click quart scroll flask to view a picture of a quart sized scroll flask with a double-ring finish. This quart scroll also has an iron pontil scar, is classified as GIX-1 or 2, and likely dates from the mid to late s. A colorful grouping of five scroll flasks dating from the late s to late s is also shown at the top of this section above. Another very popular style of completely dating site g figured flask is referred to as the "sunburst" flask, which encompasses various types based on the molded design on the body.

    Sunburst flasks are among some of the oldest of the figured flasks dating as early as to and as late as the s for a few. Most are believed to have been primarily made by various New England glass works. Sunburst flasks were made in only pint and half-pint sizes. They all have pontil scars - either glass-tipped or blowpipe types - indicating early manufacture. Colors can vary somewhat widely, though the large majority are in shades of olive green and olive amber, various other true greens, shades of amber, and aqua.

    Finishes are typically straight sheared or cracked-off or subtle variations like the rolled, flare, or globular flare typically with with obvious re-firing; and occasionally with hard to classify variations of the double ring, mineral, or others. For more information on sunburst flasks check out the following external link: Click on the following links for more pictures of this flask: As an example of how a given type of bottle can be used or re-used for a non-type typical product, click on the following links: This shows an example of this same type sunburst flask that was used or more likely re-used for "SPTS.

    Spirits of camphor was historically used internally an expectorant and still is used externally muscle aches and pains though is now considered to be a more or less hazardous substance if ingested. It is definitely not a liquor though it has "spirits" in the name. The pint, clear green sunburst flask pictured to the right is an earlier product of same Keene, NH. These flasks are often called "two pounders" by collectors as they are almost decanter-like with heavy glass weighing between 2 and 3 pounds.

    Click the following links to view more pictures of this flask: Some of these flasks have an eagle design instead of the urn on the reverse, but are otherwise very similar. The symbols of the cornucopia and urn were easily recognized during the time as symbolic of the young country's U.

    Cornucopia flasks were made in only the pint and half-pint sizes. These flasks seem to all have pontil scars - typically either a glass-tipped or blowpipe pontil - reflecting their early manufacturing dates; iron pontils are unusual.

    Colors are once again variable but dominated by olive green, olive amber, other shades of amber and green, and aqua. Finishes are almost always a of the straight sheared or cracked-off varieties or subtle variations like the rolled, flare, or globular flare typically with with obvious re-firing.

    The pictured flask both sides shown - cornucopia side to above left; urn to right is a product of Coventry Glass Works, Coventry, CT.

    These flasks are very rare, very early s or early sunusual, and unlikely to be encountered. Thus they are not covered. Users can also find some information on these type flasks, including pictures, at the following link: These could also be considered as "historical" flasks by some Munsey Most Masonic flasks have some type of design on the reverse that features an American eagle. These types of flasks are some of the earlier of the figured flasks dating primarily between and the s though a few date as late as the Civil War.

    One of the later type Masonic flasks is covered in the calabash section. These earlier Masonic flasks were only made in pint and less frequently, half-pint sizes. Like most figured flasks, the Masonic flasks can be found in a wide range of colors though most were produced in different shades of aqua, amber, and green olive green, blue-green, olive amber.

    All of these earlier Masonic flasks are pontil scarred, usually of the glass-tipped or blowpipe type. Iron pontils are rare or possibly unknown empirical observations. Finishes are usually straight shearedcracked-off, or rolled with occasional double ring or other simple applied finishes. The above pictured blue-green Masonic flask has a stylized eagle embossed on the reverse and dates between and about It was made in a two-piece hinge mold, has vertically ribbed sides, and a glass-tipped pontil scar on the base.

    Click on the following links for various view images of this flask: It was also made at the same Keene glassworks as the previous flask, though a decade or more later. Click Masonic-eagle reverse to see the other side of this flask. Another shape type variation of Masonic-eagle flask - and a common flask shape during the s, s and s - is pictured to the right. Historical Flasks This grouping of flasks is quite varied as to embossing, design, and shape.

    The unifying theme of these flasks - and what differentiates these flasks from other groups - is their historical connection be it emblematic, symbolic, or human. The most popular image on figured flasks is not surprisingly the American eagle - often embossed on both sides of the flask. The diversity of different types of eagles is amazing, ranging from the bold and artistic eagles like shown to the right to stiff and simplistic eagles like shown at this link - Pike's Peak-eagle flask reverse view.

    In general, the more detailed and artistically pleasing eagles are on the earlier flasks s to s and the more simplistic ones on the later flasks s and s though there are exceptions of course Munsey Eagles or other symbols of the U.

    Because of this shapes, sizes, finishes, mold types, and manufacturing processes vary as widely as the period allows with no particular diagnostic features unique to the group like some of the other figured flask types.

    The flask pictured above is a "beaded edge" Washington-Eagle flask GI-2 that dates from the s or s and was likely made by an early Pennsylvania glass company. Click on the following links to view more images of this flask: The reverse of this flask features a bust of George Washington and is pictured below. Another variation of the American eagle were the quite artistic versions found on the flasks produced by several Connecticut glass factories. It classifies as GII, has a smooth cup-bottom mold conformation a very unusual mold type for the eraand a crudely applied double ring finish.

    These flasks were produced using both pontil rods pontil scarred as well completely dating site g a snap-case tools smooth base. Yet another variation of the American eagle is found on an assortment of highly ornate flasks that may have been made by one of the Louisville, KY. This pint flask similar examples also were produced in quart and half gallon sizes has a blowpipe pontil scar, was blown in a two-piece key mold, and is classified as GII The likeness of many people are emblazoned on the sides of figured flasks.

    However, none were as popular as George Washington with at least 72 flasks bearing his likeness. Flasks in this category are a mixed lot with little physical commonality except that they are flasks and made during the figured flask period of to or so. Colors, shapes, sizes, finishes, and other manufacturing methods vary as widely as the period allows.

    There are even a few late 19th century flasks that were produced for Presidential elections Grover Cleveland, William Jennings Bryan, William McKinley that are cataloged within this group. The flask pictured to the right is a Washington-Eagle flask GI-2 that was discussed above with links to more pictures of the item. Some of the most common flasks in this category are the Washington-Taylor series of flasks, which contains at least 37 different examples.
    Acknowledgements Introduction his document discusses the way radiometric dating and stratigraphic principles are used to establish the conventional geological time scale.

    It is not about the theory behind radiometric dating methods, it is about their application, and it therefore assumes the reader has some familiarity with the technique already refer to "Other Sources" for more information.

    As an example of how they are used, radiometric dates from geologically simple, fossiliferous Cretaceous rocks in western North America are compared to the geological time scale. To get to that point, there is also a historical discussion and description of non-radiometric dating methods.

    A common form of criticism is to cite geologically complicated situations where the application of radiometric dating is very challenging. These are often characterised as the norm, rather than the exception. I thought it would be useful to present an example where the completely dating site g is simple, and unsurprisingly, the method does work well, to show the quality of data that would have to be invalidated before a major revision of the geologic time scale could be accepted by conventional scientists.

    Geochronologists do not claim that radiometric dating is foolproof no scientific method isbut it does work reliably for most samples.

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    It is these highly consistent and reliable samples, rather than the tricky ones, that have to be falsified for "young Earth" theories to have any scientific plausibility, not to mention the need to falsify huge amounts of evidence from other techniques. This document is partly based on a prior posting composed in reply to Ted Holden.

    My thanks to both him and other critics for motivating me. Background Stratigraphic Principles and Relative Time Much of the Earth's geology consists of successional layers of different rock types, piled one on top of another. The most common rocks observed in this form are sedimentary rocks derived from what were formerly sedimentsand extrusive igneous rocks e.

    The layers of rock are known as "strata", and the study of their succession is known as "stratigraphy". Fundamental to stratigraphy are a set of simple completely dating site g, based on elementary geometry, empirical observation of the way these rocks are deposited today, and gravity. A few principles were recognized and specified later.

    An early summary of them is found in Charles Lyell's Principles of Geologypublished inand does not differ greatly from a modern formulation: The principle of superposition - in a vertical sequence of sedimentary or volcanic rocks, a higher rock unit is younger than a lower one.

    The principle of original horizontality - rock layers were originally deposited close to horizontal. The principle of original lateral extension - A rock unit continues laterally unless there is a structure or change to prevent its extension. The principle of cross-cutting relationships - a structure that cuts another is younger than the structure that is cut.

    The principle of inclusion - a structure that is included in another is older than the including structure. The principle of "uniformitarianism" - processes operating in the past were completely dating site g by the same "laws of physics" as operate today.

    Note that these are principles. In no way are they meant to imply there are no exceptions. For example, the principle of superposition is based, fundamentally, on gravity. In order for a layer of material to be deposited, something has to be beneath it to support it. It can't float in mid-air, particularly if the material involved is sand, mud, or molten rock. The principle of superposition therefore has a clear implication for the relative age of a vertical succession of strata.

    There are situations where it potentially fails -- for example, in cave deposits. In this situation, the cave contents are younger than both the bedrock below the cave and the suspended roof above. However, note that because of the " principle of cross-cutting relationships"careful examination of the contact between the cave infill and the surrounding rock will reveal the true relative age relationships, as will the "principle of inclusion" if fragments of the surrounding rock are found within the infill.

    Cave deposits also often have distinctive structures of their own e. These geological principles are not assumptions either. Each of them is a testable hypothesis about the relationships between rock units and their characteristics.

    They are applied by geologists in the same sense that a "null hypothesis" is in statistics -- not necessarily correct, just testable. In the last or more years of their application, they are often valid, but geologists do not assume they are. They completely dating site g the "initial working hypotheses" to be tested further by data. Using these principles, it is possible to construct an interpretation of the sequence of events for any geological situation, even on other planets e.

    The simplest situation for a geologist is a "layer cake" succession of sedimentary or extrusive igneous rock units arranged in nearly horizontal layers. In such a situation, the " principle of superposition" is easily applied, and the strata towards the bottom are older, those towards the top are younger. Sedimentary beds in outcrop, a graphical plot of a stratigraphic section, and a "way up" indicator example: For example, wave ripples have their pointed crests on the "up" side, and more rounded troughs on the "down" side.

    Many other indicators are commonly present, including ones that can even tell you the angle of the depositional surface at the time "geopetal structures""assuming" that gravity was "down" at the time, which isn't much of an assumption: In more complicated situations, like in a mountain belt, there are often faults, folds, and other structural complications that have deformed and "chopped up" the original stratigraphy. Despite this, the "principle of cross cutting relationships" can be used to determine the sequence of deposition, folds, and faults based on their intersections -- if folds and faults deform or cut across the sedimentary layers and surfaces, then they obviously came after deposition of the sediments.

    You can't deform a structure e. Even in complex situations of multiple deposition, deformation, erosion, deposition, and repeated events, it is possible to reconstruct the sequence of events. Even if the folding completely dating site g so intense that some of the strata is now upside down, this fact can be recognized with "way up" indicators. No matter what the geologic situation, these basic principles reliably yield a reconstructed history of the sequence of events, both depositional, erosional, deformational, and others, for the geology of a region.

    This reconstruction is tested and refined as new field information is collected, and can be and often is done completely independently of anything to do with other methods e.

    The reconstructed history of events forms a "relative time scale", because it is possible to tell that event A occurred prior to event B, which occurred prior to event C, regardless of the actual duration of time between them. Sometimes this study is referred to as "event stratigraphy", a term that applies regardless of the type of event that occurs biologic, sedimentologic, environmental, volcanic, magnetic, diagenetic, tectonic, etc.

    These simple techniques have widely and successfully applied since at least the early s, and by the early s, geologists had recognized that many obvious similarities existed in terms of the independently-reconstructed sequence of geologic events observed in different parts of the world. One of the earliest relative time scales based upon this observation was the subdivision of the Earth's stratigraphy and therefore its historyinto the "Primary", "Secondary", "Tertiary", and later "Quaternary" strata based mainly on characteristic rock types in Europe.

    The latter two subdivisions, in an emended form, are still used today by geologists. The earliest, "Primary" is somewhat similar to the modern Paleozoic and Precambrian, and the "Secondary" is similar to the modern Mesozoic. Another observation was the similarity of the fossils observed within the succession of strata, which leads to the next topic.

    Biostratigraphy As geologists continued to reconstruct the Earth's geologic history in the s and early s, they quickly recognized that the distribution of fossils within this history was not random -- fossils occurred in a consistent order. This was true at a regional, and even a global scale.

    Furthermore, fossil organisms were more unique than rock types, and much more varied, offering the potential for a much more precise subdivision of the stratigraphy and events within it.

    The recognition of the utility of fossils for more precise "relative dating" is often attributed to William Smith, a canal engineer who observed the fossil succession while digging through the rocks of southern England. But scientists like Albert Oppel hit upon the same principles at about about the same time or earlier. In Smith's case, by using empirical observations of the fossil succession, he was able to propose a fine subdivision of the rocks and map out the formations of southern England in one of the earliest geological maps Other workers in the rest of Europe, and eventually the rest of the world, were able to compare directly to the same fossil succession in their areas, even when the rock types themselves varied at finer scale.

    For example, everywhere in the world, trilobites were found lower in the stratigraphy than marine reptiles. Dinosaurs were found after the first occurrence of land plants, insects, and amphibians. Spore-bearing land plants like ferns were always found before the occurrence of flowering plants. The observation that fossils occur in a consistent succession is known as the "principle of faunal and floral succession".

    The study of the succession of fossils and its application to relative dating is known as "biostratigraphy". Each increment of time in the stratigraphy could be characterized by a particular assemblage of fossil organisms, formally termed a biostratigraphic "zone" by the German paleontologists Friedrich Quenstedt and Albert Oppel. These zones could then be traced over large regions, and eventually globally. Groups of zones were used to establish larger intervals of stratigraphy, known as geologic "stages" and geologic "systems".

    The time corresponding to most of these intervals of rock became known as geologic "ages" and "periods", respectively. By the end of the s, most of the presently-used geologic periods had been established based on their fossil content and their observed relative position in the stratigraphy e.

    These terms were preceded by decades by other terms for various geologic subdivisions, and although there was subsequent debate over their exact boundaries e. By the s, fossil succession had been studied to an increasing degree, such that the broad history of life on Earth was well understood, regardless of the debate over the names applied to portions of it, and where exactly to make the divisions.

    All paleontologists recognized unmistakable trends in morphology through time in the succession of fossil organisms. This observation led to attempts to explain the fossil succession by various mechanisms. Perhaps the best known example is Darwin's completely dating site g of evolution by natural selection.

    Note that chronologically, fossil succession was well and independently established long before Darwin's evolutionary theory was proposed in Fossil succession and the geologic time scale are constrained by the observed order of the stratigraphy -- basically geometry -- not by evolutionary theory. Calibrating the Relative Time Scale For almost the next years, geologists operated using relative dating methods, both using the basic principles of geology and fossil succession biostratigraphy.

    Various attempts were made as far back as the s to scientifically estimate the age of the Earth, and, later, to use this to calibrate the relative time scale to numeric values refer to "Changing views of the history of the Earth" by Richard Harter and Chris Stassen.

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    Most of the early attempts were based on rates of deposition, erosion, and other geological processes, which yielded uncertain time estimates, but which clearly indicated Earth history was at least million or more years old. A challenge to this interpretation came in the form of Lord Kelvin's William Thomson's calculations of the heat flow from the Earth, and the implication this had for the age -- rather than hundreds of millions of years, the Earth could be as young as tens of million of years old.

    This evaluation was subsequently invalidated by the discovery of radioactivity in the last years of the 19th century, which was an unaccounted for source of heat in Kelvin's original calculations. With it factored in, the Earth could be vastly older. Estimates of the age of the Earth again returned to the prior methods. The discovery of radioactivity also had another side effect, although it was several more decades before its additional significance to geology became apparent and the techniques became refined.

    Because of the chemistry of rocks, it was possible to calculate how much radioactive decay had occurred since an appropriate mineral had formed, and how much time had therefore expired, by looking at the ratio between the original radioactive isotope and its product, if the decay rate was known. Many geological complications and measurement difficulties existed, but initial attempts at the method clearly demonstrated that the Earth was very old.

    In fact, the numbers that became available were significantly older than even some geologists were expecting -- rather than hundreds of millions of years, which was the minimum age expected, the Earth's history was clearly at least billions of years long.

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    Radiometric dating provides numerical values for the age of an appropriate rock, usually expressed in millions of years. Therefore, by dating a series of rocks in a vertical succession of strata previously recognized with basic geologic principles see Stratigraphic principles and relative timeit can provide a numerical calibration for what would otherwise be only an ordering of events -- i.

    The integration of relative dating and radiometric dating has resulted in a series of increasingly precise "absolute" i. Given the background above, the information used for a geologic time scale can be related like this: How relative dating of events and radiometric numeric dates are combined to produce a calibrated geological time scale.

    In this example, the data demonstrates that "fossil B time" was somewhere between and million years ago, and that "fossil A time" is older than million years ago.
    When personally reviewing all of the top dating sites for meeting older women we look at a huge number of variables. We strive to identify the sites that our readers will find the most success using.

    To ensure that we provide a fair and balanced take we always measure each site on the following characteristics and many other: These numbers come from publicly released numbers and are critical to consider. The best dating sites for meeting older women have millions of men and women using their site.

    The larger the membership the easier it is to meet a woman.

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    The higher the concentration of cougars the better. Even if a site has a lot of people using it you may not find great success if there are completely dating site g few actual older women using the site. Combining a high total membership and high cougar concentration makes for a great site for cougar dating. Free cougar dating sites are notorious for their extremely low success rates and a lot are scams.

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    A few of the free cougar dating reviews sites are listed further down in this post. Legitimate — No matter where you spend your time you need to ensure the site is run by a well known legitimate company. There are a lot of sites out there that look decent at the beginning but really are just shells covering up empty sites that only want to take your money. Profile setup time — The top cougar dating sites out there know that it has to be easy to make a profile on their site.

    Therefore, how long will it takes to fully set up your profile and be ready talk to older women or cougars get up and running to meet you is critical. This includes the signup, profile completion, and any other questions that are required to get started. More in-depth profiles can create higher commitment levels for cougars. It also makes it easier to identify a woman who is interested in dating younger men.

    If there are a lot of cubs around it can have the huge benefit or regularly attracting a lot of cougars. While it might be tempting to think that you want to be the only option, in reality it is in your best interest to have a healthy number of other guys out there.

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    Plus, it keeps you from getting to lazy! Daily time commitment — How much of a daily time commitment is necessary to be successful on this site?

    One of the best things about dating older women online is the minimum commitment. Once you set up a great profile it will only require a few minutes a day to get in touch with dozens of cougars. Some cougar dating sites provide automated matching while other require you to do that on your own.

    The technological capabilities, matchmaking algorithms, and user interface of a site all have huge impacts on how much time it actually takes to meet a cougar. Success Guarantee — Does the site provide some kind of guarantee that you will be successful?

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    These guarantees of often in the form of additional months of free membership but require certain conditions to have been met during the initial membership period to qualify.

    These conditions can include logging in a certain number of times, completely filling out a profile, or messaging a certain number of older women.

    A success guarantee is a huge indicator that you are dealing with a quality site and should give you a little more confidence that you are not wasting your time. Now that we have identified WHERE you will be looking for cougars online lets discuss a little more about WHY online dating is a must for anyone aspiring to date older women.

    If you set off to find a cougar on any given day your results will be hit or miss. Even if you do happen to find a woman to pursue the circumstances are often difficult. The more older women you meet the better your understanding of what you want. There is no easier method to meet a lot of older women than harnessing the power of the internet.

    Where else can you spend a few minutes a day and potentially meet completely dating site g of attractive older women? Even men who are comfortable meeting and talking to women their own age are not safe. It is a much more comfortable learning process when you have the time to think about what you are going to say. Using online message or text you build a level of comfort with a cougar before meeting her in the real world.

    You have nothing to lose by trying online dating aside from a little time. In the time it would take shower, get dressed, and drive down to the local cougar bar you can complete your profile and have messaged a dozen attractive cougars. For the cost of a few drinks at the bar you can join eHarmonyElite Singles, and Cougar Life and stop wasting time and money buying drinks in bars.

    It is the most efficient way to meet older women imaginable. Where else can you quickly find and talk to a huge number of beautiful, successful, and pre-qualified older women that are eager to meet younger men.

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    Can you imagine how long it would take in a bar, even a notorious cougar hang out, to meet and have a conversation with 20 attractive cougars? You can achieve the same goals in ten minutes online! Meeting woman in the usual places should still be a regular part of your cougar dating strategy.

    There is absolutely no reason why every single man should not be using online dating. Now that we understand what the cubs are getting out of these sites. We are dealing with women who are not only more mature and sophisticated than the girls young men are used to dealing. While your average year-old is working at Starbucks or searching for entry level jobs cougars are busy with the career they have spent years building.

    These women do not have time to spend in bars looking for younger men, nor do they want to. They are very open to finding mature younger men from the comfort of their own homes however. Discretion Online dating no longer has any stigma attached to it.

    Having a public profile on eHarmonyEliteSingles. Most people would not even bat an eye about it. However, having a profile on some of the extremely sketchy dating sites listed below could be damaging to the reputation she has spent many years building. There is often the assumption that men desire to only date women younger than them.

    Being able to quickly and easily see from a profile that a man is interested in dating women older than them makes it much easier for a woman to make the first move. No public member counts If the site is unwilling to share the number of members they have it is typically because those numbers are small and would make them look bad. It is a big problem if a site is trying to hide any information.

    The top cougar dating sites out there proudly advertise the number of satisfied customers they have. There are a lot of sites out there that are nearly completely men with almost no women. Lots of stock photography of nearly naked women everywhere but the profiles If the homepage is very clearly only going targeting men you can assume that men are their core audience.

    Do you want to join a cougar dating site that is only trying to attract men as members? A good site will try very hard to attract both men and older women. They know that sites without a good balance are not going to last very long. Unlicensed picture of famous celebrity couples Ashton Kutcher and Demi Moore were an inspirational couple for all the cougars and cubs out there.

    As you can see from the long list of dating websites above there are a TON completely dating site g extremely sketchy websites on the internet. The twelve I listed above are just a small sample of what you can find with a simple Google search.

    You need to use your instincts and common sense when choosing which websites to frequent. However, if you are a busy man or simply someone who likes to be efficient and effective with his time take a few minutes and sign up for eHarmony, Elite Singles, and Cougar Life. These cougar dating websites have a fantastic population of older completely dating site g looking to meet younger men. If you are serious about dating cougars there is nothing you will find that will yield better results for the amount of effort you put in.

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