letha weapons Un Official Fan Site Tribute

letha weapons : This Is An Un Official Fan Site Tribute
Leatha Weapons, Leathal Weapons, Leetha Weapons, Leaha Weapons, Letha Weapon, Lethal Weapons, Leatha Leathal Weapons, Leatha Weapons, Leetha Weapons
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letha weapons

PERFORMER AKA Leathal Weapons, Leatha Weapons, Leetha Weapons BIRTHDAY July 05, 1972 (47 years old) ASTROLOGY Cancer BIRTHPLACE Louisiana, USA YEARS ACTIVE 1994-2000 (Started around 22 years old)
Letha Weapons (born 5 July 1972) is an adult model and former porn actress who appeared in many adult films in the big-bust category. Career Letha appeared in over 50 adult videos over the course of her adult career, which began in 1994. Letha has also made appearances in shock jock Howard Stern's movie Butt Bongo Fiesta, where she played the "Queen of the Jungle", amongst other things. She also appeared on the television series Married... with Children as a dancer named Rocki Mountains in the Jiggly Room. She has made other appearances on Sally Jessy Raphael and The Richard Bey Show.

John Wayne Bobbitt Uncut adult video Letha appeared in the 1994 adult video John Wayne Bobbitt Uncut, featuring the pornographic debut of John Wayne Bobbitt,[1] whose penis was severed in a knife attack by his then wife.[3] Other appearances Russ Meyer described Weapons's breasts in his autobiography, A Clean Breast: The Life and Loves of Russ Meyer as "Big boobs bolstered by a breast hammock based on the principle that made the Sydney Opera House feasible".[4] The augmented size of Weapon's breasts has also been derided by critics. 1996 Unknown AVN Halloween Sex-fest 1997 Eurotique Entertainment NonSex 1 O Big Boob Bangeroo 8 1997 Totally Tasteless Facial 1 DO Big Boob Bangeroo 9 1997 Totally Tasteless Facial DO Big Boob Bikini Bash 1995 Big Top Video NonSex DRO Big Boob Brunettes 2006 Cinderella DO Big Boobs in Buttsville 1997 Ultimate Video Anal Facial A2M 4 DRO Big Bust Babes 23 1994 AFVC Big Bust Babes 39 1996 AFVC Big Bust Bangers 2 1994 Fantastic Pictures Facial IR Big Knockers 11 1995 Topper Video Inc. MastOnly 1 O Big Knockers 5 1994 Topper Video Inc. MastOnly O Big Tit Racket 1995 Pepper Productions Big Tits Galore 2003 Totally Tasteless DO Big Ums 1995 Glitz Video Blue Balls 1995 Leisure Time Entertainment O Blue Ribbon Butt Fucks 3 2007 Seymore Butts 1 DO Body Of Love 1994 K-Beech Video 1 Boob Tube Lube 1997 Raw Silk Boobs A Poppin' 1 1994 Totally Tasteless Facial 1 DO Boobsville Banger Girls 3 2004 Big Top Video DO Booby Prize 1995 Pepper Productions D Bosom Buddies 1 1995 Score LezOnly Breastman's Wet T-shirt Contest 1994 Erotic Video Network 1 Breasts Of Breastman 1997 Erotic Video Network Busty Kittens 1999 Napali Video NonSex O Candy Store 1999 VCA DO Coming Out Bi 1995 Metro IR DO Der Champion 1995 Big Top Video DO Dick and Jane Do the Strip 1994 Avica Entertainment NonSex Dirty Words 2002 Flesh Entertainment Double D Dykes 27 1996 Gourmet Video Collection LezOnly Double D Reunion 1995 Big Top Video MastOnly DRO Duke of Knockers 2 1995 Big Top Video Facial DO Fantasy Lover 1995 Venus 99 Formal Affair (new) 1994 Leisure Time Entertainment Freeway Love 1994 Fat Dog Full House 2 2006 Blue Coyote Pictures DO Gang Bang Bitches 16 1997 Plum Productions Facial 1 Gang Bang Cum Shots 1 1994 Fantastic Pictures Girls Around The World 15 1994 Big Top Video NonSex Girls Around the World 22 1995 Big Top Video Glitz Tits 8 1994 Glitz Video Harlots From Hooterville 1994 Blue Coyote Pictures Helen's Beauties 6: Deadly Weapon 1995 Blue Coyote Pictures Hollywood Backside 6 1995 Unknown Hollywood Starlet Search 1994 Sin City Humongous Hooters 1994 Napali Video NonSex O John Wayne Bobbitt Uncut 1994 Leisure Time Entertainment 1 DO Lesbian Castle 1994 Lipstik Video LezOnly O Lipstick Lesbians 5: Lesbian Orgy 1998 Zane Entertainment Group LezOnly 1 O Mellon Man 1994 Avica Entertainment DO Monster Tits 2004 Leisure Time Entertainment DO Mountie 1994 Plum Productions 1 O Mystique 1996 Sin City LezOnly 1 O Nip/Fuck 2000 VCA IR DO On Location in Palm Springs 1996 Big Top Video NonSex On Location In The Bahamas 1996 Big Top Video NonSex The Ruhpolding Formation is a sedimentary formation of the Northern Calcareous Alps deposited during the Upper Jurassic. The open marine radiolarite is very rich in silica. Only the Best of Seymore Butts 6 2001 Seymore Butts 1 DRO Philmore Butts Strikes Gold 1996 Sunshine Films DO Raging Passions 1996 Infinity Film And Video Red Hot For Sex 1996 Red Hot Video Rodney Blasters 1 1995 L.B.O. Entertainment Facial DO Rodney Moore's How To Make A Model 4 1994 L.B.O. Entertainment Facial Savage Fury 3 1994 Leisure Time Entertainment Facial O She's No Angel 2 1995 Infinity Film And Video Switch Hitters 8 1995 Metro Ten Years of Big Busts 4 2000 Big Top Video DO Tit to Tit 3 1996 Big Top Video LezOnly DRO Try It, You'll Bi It 2009 Metro DO Watch Me Pee 2000 Leisure Time Entertainment Facial 1 O Way They Wuz 1996 Shooting Star Video Wise Cracks 2001 Seymore Butts Anal Faci The Ruhpolding Formation derives its name from its type locality Ruhpolding, a commune in Upper Bavaria situated at the edge of the Northern Calcareous Alps. The type locality, situated southwest of Ruhpolding (at Gschwendlbach near Röthelmoos, Urschlau) is a bad choice as it doesn't show the characteristic red radiolarites found elsewhere in the Austroalpine domain but only grey to red cherty limestones.[1] This is the reason why Gawlik (2000) suggested a new type profile with a complete development of the radiolarite at Mörtlbach northeast of Hallein.[2] The formation is also known as Ruhpolding Radiolarite[3] or Ruhpolding Beds.[4] In a wider context all the radiolarites of Late Bajocian, Callovian, Oxfordian, Kimmeridgian and Early Tithonian age are reunited within the Ruhpolding Radiolarite Group (RRG). Occurrence The type locality of the Ruhpolding Formation belongs to the Lechtal Nappe of the Bajuvaric Unit, one of the major tectonic subdivisions of the Northern Calcareous Alps. The occurrence of the formation extends from the Allgäu Alps in the west via the Lechtal Alps to the Chiemgau Alps in the east. The Ruhpolding Formation is also found in the Tirolic Unit to the south of the Bajuvaric Unit and therefore extends into the eastern part of the Northern Calcareous Alps. The Ruhpolding Radiolarite Group is encountered in the Southern Alps and even in the Penninic domain (Piemont Zone). Stratigraphy Within the Bajuvaric Unit the Ruhpolding Formation conformably overlies the Chiemgau Beds, further west in the Allgäu Alps it overlies the upper Allgäu Beds. It is conformably overlain by the so-called Aptychus Limestone of the Ammergau Formation. The changeover to the Aptychus Limestone is gradual. The lower contact of the Ruhpolding Formation is very distinct and outlined by a several centimeter thick bedding joint.[5] – as can be seen in the Tauglboden Basin of the northern Tirolic Unit where the Ruhpolding Formation overlies the red limestone of the Klaus Formation. In the Tauglboden Basin the Ruhpolding Formation is followed by the Tauglboden Formation of Kimmeridgian and lower Tithonian age. In the Sillenkopf Basin of the southern Tirolic Unit the Ruhpolding Formation is underlain by the Strubberg Formation and overlain by the Sillenkopf Formation which was deposited at the same time as the Tauglboden Formation. Lithology Various radiolarians under the microscope Lithologically the up to 50 meter thick Ruhpolding Formation consists of black-green to red radiolarites grading into cherty limestones, cherty marls and cherty shales. It has formed from radiolarian ooze. The ooze consolidated diagenetically to thinly layered and regularly banded cherts. The chert layers are usually separated by very thin claystone layers creating a cyclic appearance. This cyclicity might correlate with Milankovic cycles. A plausible diagenetic cause can be excluded due to slump structures that incorporate several individual cycles. The cherts are mainly earthy red, but show greenish-blackish hues in places. The red coloration due to hematite is caused by the complete oxidation of iron compounds in oxygen-rich bottom waters. The red layers show Fe3+/Fe2+ > 1, whereas in the greenish layers the ratio is < 1, the coloration in the latter being tied to sericite, chlorite and maybe pyrite. In thin section it can be observed that the siliceous groundmass is derived from the innumerable skeletons of radiolarians (maximal size 0.1 mm in diameter) altered during diagenesis. The cherts chemical composition nearly approaches 100% silica. On a macroscopic scale the rock is intensely criss-crossed by net-like fracture systems, which were later filled by calcite. These fractures were opened by tectonic stresses judging from structures like tension gashes. Tuff layers can be encountered right at the very base of the formation. They are probably a precursor of the later ehrwaldite magmatism. Fossils The Ruhpolding Formation consists mainly of microfossils, the bulk being made up by radiolarians. Macrofossils are extremely rare apart from some aptychi, crinoids like Saccocoma, spicules and filaments. Benthic foraminifera can occasionally be found but planktonic foraminifera are completely absent.[6] Amongst the abundant radiolarians the following taxa are present: Nassellaria – Amphipyndacidae: Triversus Nassellaria – Archaeodigtyomitridae: Archaeodictyomitra Nassellaria – Eucyrtidiidae: Stichocapsa Nassellaria – Hsuidae: Hsuum Nassellaria – Parvicingulidae: Parvicingula Nassellaria – Williriedellidae: Williriedellum Nassellaria – : Tricolocapsa Spumellaria – Angulobracchiidae: Paronaella Depositional environment The fully marine Ruhpolding Formation was deposited in the pelagic domain at the northern edge of the Neotethys ocean, as indicated by rare ammonite finds like Hibolites semisulcatus. The water depth of deposition is still disputed. Today radiolarian oozes form below the carbonate compensation depth (CCD) at 4,000 to 5,000 metres (13,000 to 16,000 ft) water depth. In the Upper Jurassic the CCD was probably much higher and ranged somewhere between 2,000 and 3,000 metres (6,600 and 9,800 ft) depth due to a greatly diminished calcareous nanoplankton at that time. The radiolarian blooms probably were triggered by volcanism and/or changing circulation patterns. The required silica was provided by volcanic exhalations and/or by upwelling.[7] Ruhpolding turning point The sedimentation of the radiolarites represents a sudden and drastic change in the sedimentation history of the Northern Calcareous Alps. This event was termed the Ruhpolding turning point (Ruhpoldinger Wende in German). It was a decisive and not a transient, repetitive change, because the deep-water radiolarites and later Aptychen Beds clearly differ in character from the lower and mid-Jurassic sediments. During the Dogger the turning point was preceded by a rapid drop in sedimentation rates and ensuing thicknesses. This is exemplified by the increasing number of omission surfaces in the upper Klaus-Formation combined with a general slowed-down and more patchy sedimentation. This starved sediment supply is probably due to a continuous deepening of the basin. The turning point is also marked by tectonic movements enhancing the topographic differences of the seafloor. For instance already existing topographic highs were raised into shallow water. On these raised areas the Ruhpolding radiolarites did not accumulate; instead red limestones like the Agathakalk or the Hasselberg Limestone continued to be deposited here. This tectonically accentuated profile was slowly levelled later during the sedimentation of the Aptychen Beds. Another characteristic of the Ruhpolding turning point is the associated volcanic activity. The tuff layers right at the onset of the Ruhpolding formation are without doubt the precursors of the Upper Jurassic magmatic pulse in the Alps.[8] Also noticeable is a pronounced increase in autokinetic sediments like turbidites, debris flows, slides etc. at or near the turning point. Good examples are the limestones of the Barmstein, the Sonnwendbreccia, the Tauglboden Formation and the Strubberg Formation. The gradual replacement of the radiolarian oozes of the Ruhpolding Formation by coccolith oozes of the overlying Aptychen Beds can be explained by further deepening of the basin and/or by blooming calcareous nanoplankton.

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