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MAGMATIC PM-DMX1 is an optional pan motor accessory for the MAGMATIC CRISP MAX Snow Machine. Install the output nozzle of the Crisp Max, using the included mounting bracket, onto the PM-DMX1 to precisely control 120 degrees of pan movement via DMX-512 or manually using the 4-button LED control panel menu display on the unit. The PM-DMX1 features 2 DMX channel modes, 0-120 degree position index movement and 3 different degree internal auto-pan programs (60 Degree , 90 Degree , 120 Degree ) each having 5 speed settings, a pan inversion mode which inverts the pan movement, primary / secondary modes, 5pin DMX in/out for easy control connection and linking multiple units, an included mounting bracket that better balances weight distribution of the Crisp Max nozzle unit, mini-omega bracket so PM-DMX1 can be clamped and /truss mounted, and a 100-240V auto switching power supply.

Magmatic sulfides provide most of the world's supplies of platinum and nickel, among other rare and valuable ores. The author, a ranking authority on the topic, discusses the types of rocks that contain magmatic sulfides, the chemical processes by which they form, and the geological setting of major nickel-copper and platinum deposits throughout the world--in Canada, Australia, the U.S.S.R., South Africa, the U.S.A., and Zimbabwe. Naldrett also examines how theories about ore genesis can be applied in exploring for minerals. The book will be used in graduate-level courses and by economic geologists, geochemists, and geologists in the mining industry. It will also be of interest to members of geological surveys worldwide.

<font size='5'>Kernom MOHO Magmatic Fuzz Station Pedal</font><br/><br/><p>The <strong>Kernom MOHO Magmatic Fuzz...

High-volume Snow Machine with LCD Touch Screen and DMX Control.

High-power Snow Machine with Snow Cannon Adjustable Flake Size Air Pump Fan Road Case and DMX and RDM Control.

Magmatic sulfides provide most of the world's supplies of platinum and nickel, among other rare and valuable ores. The author, a ranking authority on the topic, discusses the types of rocks that contain magmatic sulfides, the chemical processes by which they form, and the geological setting of major nickel-copper and platinum deposits throughout the world--in Canada, Australia, the U.S.S.R., South Africa, the U.S.A., and Zimbabwe. Naldrett also examines how theories about ore genesis can be applied in exploring for minerals. The book will be used in graduate-level courses and by economic geologists, geochemists, and geologists in the mining industry. It will also be of interest to members of geological surveys worldwide.

This book offers a high-level summary of shallow magmatic systems (dykes, sills and laccoliths) to support geoscience master and PhD students, scientists and practicing professionals. The product of the LASI (Laccoliths and Sills conference) workshop, it comprises thematic sections written by one or more experts on the respective field. It features reviews concerning the physical properties of magma, geotectonic settings, and the structure of subvolcanic systems, as well as case studies on the best-known systems. The book provides readers a broad and comprehensive understanding of the subvolcanic perspective on pluton growth, which is relevant for mineralogical processes as well as the genesis of mineral deposits.

This book gives an up-to-date overview of the physical geology of sub-volcanic intrusions. Topics covered in this wide-ranging volume include important aspects of the field geology and physical volcanology of sills, laccoliths and sub-volcanic complexes, magma-sediment interaction and numerical and experimental studies aimed at quantifying more precisely the emplacement mechanics of high-level magmatic intrusions. Provocative papers ask whether laccoliths and high-level sills are forming today, and question the nature of the relationship between high-level intrusions and contemporaneous volcanic activity. Several contributions also deal with the more applied aspects of high-level magma emplacement and 3D seismic imaging of sill and laccolith complexes as relevant to the hydrocarbons industry. It is hoped that with the publication of this volume a consensus will emerge that will help to advance our understanding of the more important physical factors governing the emplacement of high-level intrusions in the continental crust, along with their wider geotectonic implications. Also available: Structure and Emplacement of High-Level Magmatic Systems - Special Publication no 302 - ISBN 1862392560 Dynamics of Crustal Magma Transfer, Storage and Differentiation - Special Publication no 304 - ISBN 1862392587 The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society in the world, and one of the largest publishers in the Earth sciences.The Society publishes a wide range of high-quality peer-reviewed titles for academics and professionals working in the geosciences, and enjoys an enviable international reputation for the quality of its work.The many areas in which we publish in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic studies and geochemistry-Remote sensing-History of geology-Regional geology guides

This book offers a high-level summary of shallow magmatic systems (dykes, sills and laccoliths) to support geoscience master and PhD students, scientists and practicing professionals. The product of the LASI (Laccoliths and Sills conference) workshop, it comprises thematic sections written by one or more experts on the respective field. It features reviews concerning the physical properties of magma, geotectonic settings, and the structure of subvolcanic systems, as well as case studies on the best-known systems. The book provides readers a broad and comprehensive understanding of the subvolcanic perspective on pluton growth, which is relevant for mineralogical processes as well as the genesis of mineral deposits.

This book gives an up-to-date overview of the physical geology of sub-volcanic intrusions. Topics covered in this wide-ranging volume include important aspects of the field geology and physical volcanology of sills, laccoliths and sub-volcanic complexes, magma-sediment interaction and numerical and experimental studies aimed at quantifying more precisely the emplacement mechanics of high-level magmatic intrusions. Provocative papers ask whether laccoliths and high-level sills are forming today, and question the nature of the relationship between high-level intrusions and contemporaneous volcanic activity. Several contributions also deal with the more applied aspects of high-level magma emplacement and 3D seismic imaging of sill and laccolith complexes as relevant to the hydrocarbons industry. It is hoped that with the publication of this volume a consensus will emerge that will help to advance our understanding of the more important physical factors governing the emplacement of high-level intrusions in the continental crust, along with their wider geotectonic implications. Also available: Structure and Emplacement of High-Level Magmatic Systems - Special Publication no 302 - ISBN 1862392560 Dynamics of Crustal Magma Transfer, Storage and Differentiation - Special Publication no 304 - ISBN 1862392587 The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society in the world, and one of the largest publishers in the Earth sciences.The Society publishes a wide range of high-quality peer-reviewed titles for academics and professionals working in the geosciences, and enjoys an enviable international reputation for the quality of its work.The many areas in which we publish in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic studies and geochemistry-Remote sensing-History of geology-Regional geology guides

This 4 liter concentrate makes 80 liters of ready to use Snow fluid. This concentrate is mixed at a ratio of 19:1. The Atmosity APS fluid is a premium, dry-on-impact snow fluid formulated for the Magmatic Polar series.

The ARH fluid by Atmosity is an oil-based haze fluid designed to work with the Magmatic Therma Tour 600, Therma Tour 800, or any other haze machines with a compressor system that require oil-based fluid. This fluid has been specially formulated with advanced fine particulates, which extend the atmospheric linger effect and excels at revealing light beams and mid-air effects.ARH fluid bottles are available in 2-liter, 4-liter, and 20-liter containers. This haze fluid is colorless, non-toxic, non-irritating, and it requires no dilutions and is ready for use right out of the container.

The MAGMATIC MAGRF is a 433-MHz wireless remote control that is compatible with all MAGMATIC foggers, hazers, snow machines, CO2 simulators, low lying, and bubble machines. Once the receiver unit is installed, it has an effective range of up to 150-feet with clear line-of-sight (50-meters) to manually control the output of your Magmatic machine.

The Atmosity ALL fluid is a water-based cryogenic fog fluid formulated for the Magmatic line of low-lying fog machines. It has been engineered to produce an artificial, low-lying fog effect for both indoor and outdoor applications.Atmosity ALL fog fluid bottles are available in 2-liter, 4-liter, and 20-liter containers. This fog fluid is pH balanced, colorless, non-toxic, non-irritating, and odorless, and it requires no dilutions and is ready for use right out of the container.

The MAGMATIC MAGRF-R is a 433 MHz wireless receiving card with a working distance of 150 feet. This wireless receiving card works in conjunction with the MAGRF-T and is compatible with all MAGMATIC foggers, hazers, snow machines, CO2 simulators, low lying machines, and bubble machines.

MagRemote VIDI is compatible with Magmatic's line of products, like the Therma series, Magma series, and Polar series. "Rocket Series is not fully compatible with the remote"

Introducing POLAR CRISP MAX from MAGMATIC atmospheric effects, a dependable, high-output snow machine that makes it easy to create scene-setting wintry settings. CRISP MAX is capable of producing high volumes of naturalistic snow with the capacity to adjust snowflake size for greater versatility. It includes a 20-liter fluid tank hidden inside a road case with durable casters for easier portability. The unit's 10-meter long hose can be rigged on a standard truss or tripod stand and can extend up to 30 meters horizontally or vertically.

The Atmosity Premium Haze Fluid is a water based haze fluid intended to create synthetic atmospheric effects for use with Magmatic Hazer machines - Thermatic series, or any other compressor system haze machines that require water based fluid.The Atmosity Premium Haze Fluid is a water-based haze liquid, much drier than the oil-based version. So, this liquid produces virtually no residue. It's Colorless, odorless and non-flammable.

The ARH fluid by Atmosity is an oil-based haze fluid designed to work with the Magmatic Therma Tour 600, Therma Tour 800, or any other haze machines with a compressor system that require oil-based fluid. This fluid has been specially formulated with advanced fine particulates, which extend the atmospheric linger effect and excels at revealing light beams and mid-air effects.ARH fluid bottles are available in 2-liter, 4-liter, and 20-liter containers. This haze fluid is colorless, non-toxic, non-irritating, and it requires no dilutions and is ready for use right out of the container.

The Atmosity APS fluid is a premium, dry-on-impact snow liquid formulated for the Magmatic Polar series, as well as most other water-based snow machines. The Atmosity premium snow fluid has been engineered to produce a high volume of realistic snow for both indoor and outdoor applications.Atmosity APS premium dry snow fluid bottles are available in 2-liter, 4-liter, and 20-liter containers. This snow fluid is pH balanced, colorless, non-toxic, non-irritating, and odorless, and it requires no dilutions and is ready for use right out of the container.