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    You don't see these components as separate entities, instead you see them as related and interdependent parts of a single entity.

    You want to deploy, manage, and monitor them as a group. Azure Resource Manager enables you to work with the resources in your solution as a group. You can deploy, update, or delete all the resources for your solution in a single, coordinated operation. You use a template for deployment and that template can work for different environments such as testing, staging, and production. Resource Manager provides security, auditing, and tagging features to help you manage your resources after deployment.

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    Functionality initially released through APIs will be represented in the portal within days of initial release. Choose the tools and APIs that work best for you - they have the same capability and provide consistent results.

    The API passes requests to the Resource Manager service, which authenticates and authorizes the requests. Resource Manager then routes the requests to the appropriate resource providers. Terminology If you're new to Azure Resource Manager, there are some terms you might not be familiar with. Some common resources are a virtual machine, storage account, web app, database, and virtual network, but there are many more. The resource group can include all the resources for the solution, or only those resources that you want to manage as a group.

    You decide how you want to allocate resources to resource groups based on what makes the most sense for your organization. Each resource provider offers operations for working with the resources that are deployed. Some common resource providers are Microsoft. Compute, which supplies the virtual machine resource, Microsoft. Storage, which supplies the storage account resource, and Microsoft.

    Web, which supplies resources related to web apps. It also defines the dependencies between the deployed resources. The template can be used to deploy the resources consistently and repeatedly.

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    The Resource Manager template is an example of declarative syntax. In the file, you define the properties for the infrastructure to deploy to Azure. The benefits of using Resource Manager Resource Manager provides several benefits: You can deploy, manage, and monitor all the resources for your solution as a group, rather than handling these resources individually.

    You can repeatedly deploy your solution throughout the development lifecycle and have confidence your resources are deployed in a consistent state. You can manage your infrastructure through declarative templates rather than scripts. You can define the dependencies between resources so they're deployed in the correct order.

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    You can apply access control to all services in your resource group because Role-Based Access Control RBAC is natively integrated into the management platform. You can apply tags to resources to logically organize all the resources in your subscription. You can clarify your organization's billing by viewing costs for a group of resources sharing the same tag. Resource Manager provides a new way to deploy and manage your solutions. If you used the earlier deployment model and want to learn about the changes, see Understanding Resource Manager deployment and classic deployment.

    Guidance The following suggestions help you take full advantage of Resource Manager when working with your solutions. Define and deploy your infrastructure through the declarative syntax in Resource Manager templates, rather than through imperative commands.

    Define all deployment and configuration steps in the template. You should have no manual steps for setting up your solution. Run imperative commands to manage your resources, such as to start or stop an app or machine. Arrange resources with the same lifecycle in a resource group.

    Use tags for all other organizing of resources. For guidance on how enterprises can use Resource Manager to effectively manage subscriptions, see Azure enterprise scaffold - prescriptive subscription governance.

    For recommendations on creating Resource Manager templates that you can use across global Azure, Azure sovereign clouds, and Azure Stack, see Develop Azure Resource Manager templates for cloud consistency. Resource groups There are some important factors to consider when defining your resource group: All the resources in your group should share the same lifecycle.

    You deploy, update, and delete them together. If one resource, such as a database server, needs to exist on a different deployment cycle it should be in another resource group. Each resource can only exist in one resource group.

    Terminology

    You can add or remove a resource to a resource group at any time. You can move a resource from one resource group to another group.

    For more information, see Move resources to new resource group or subscription. A resource group can contain resources that reside in different regions. A resource group can be used to scope access control for administrative actions.

    A resource can interact with resources in other resource groups. This interaction is common when the two resources are related but don't share the same lifecycle for example, web apps connecting to a database. When creating a resource group, you need to provide a location for that resource group. You may be wondering, "Why does a resource group need a location? And, if the resources can have different locations than the resource group, why does the resource group location matter at all?

    Therefore, when you specify a location for the resource group, you're specifying where that metadata is stored. For compliance reasons, you may need to ensure that your data is stored in a particular region. Resource providers Each resource provider offers a set of resources and operations for working with an Azure service. For example, if you want to store keys and secrets, you work with the Microsoft. This resource provider offers a resource type called vaults for creating the key vault.

    The name of a resource type is in the format: For example, the key vault type is Microsoft. Before getting started with deploying your resources, you should gain an understanding of the available resource providers. Knowing the names of resource providers and resources helps you define resources you want to deploy to Azure. Also, you need to know the valid locations and API versions for each resource type.

    For more information, see Resource providers and types.

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    Template deployment With Resource Manager, you can create a template in JSON format that defines the infrastructure and configuration of your Azure solution. By using a template, you can repeatedly deploy your solution throughout its lifecycle and have confidence your resources are deployed in a consistent state.

    When you create a solution from the portal, the solution automatically includes a deployment template. You don't have to create your template from scratch because you can start with the template for your solution and customize it to meet your specific needs.

    You can retrieve a template for an existing resource group by either exporting the current state of the resource group, or viewing the template used for a particular deployment. Viewing the exported template is a helpful way to learn about the template syntax. To learn about the format of the template and how you construct it, see Create your first Azure Resource Manager template. Resource Manager processes the template like any other request see the image for Consistent management layer.

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    For example, when Resource Manager receives a template with the following resource definition: For example, you can deploy your three tier application through a single template to a single resource group.

    But, you don't have to define your entire infrastructure in a single template. Often, it makes sense to divide your deployment requirements into a set of targeted, purpose-specific templates. You can easily reuse these templates for different solutions. To deploy a particular solution, you create a master template that links all the required templates. The following image shows how to deploy a three tier solution through a parent template that includes three nested templates.

    If you envision your tiers having separate lifecycles, you can deploy your three tiers to separate resource groups. Notice the resources can still be linked to resources in other resource groups.

    Consistent management layer

    For information about nested templates, see Using linked templates with Azure Resource Manager. Azure Resource Manager analyzes dependencies to ensure resources are created in the correct order.

    If one resource relies on a value from another resource such as a virtual machine needing a storage account for disksyou set a dependency. For more information, see Defining dependencies in Azure Resource Manager templates. You can also use the template for updates to the infrastructure. For example, you can add a resource to your solution and add configuration rules for the resources that are already deployed. If the template specifies creating a resource but that resource already exists, Azure Resource Manager performs an update instead of creating a new asset.

    Azure Resource Manager updates the existing asset to the same state as it would be as new.

    Welcome to TechTarget's expert community for technology professionals.

    Resource Manager provides extensions for scenarios when you need additional operations such as installing particular software that isn't included in the setup. If you're already using a configuration management service, like DSC, Chef or Puppet, you can continue working with that service by using extensions. For information about virtual machine extensions, see About virtual machine extensions and features.

    Finally, the template becomes part of the source code for your app. You can check it in to your source code repository and update it as your app evolves.

    You can edit the template through Visual Studio.
    General considerations Distinctions between relative-age and absolute-age measurements Local relationships on a single outcrop or archaeological site can often be interpreted to deduce the sequence in which the materials were assembled. This then can be used to deduce the sequence of events and processes that took place or the history of that brief period of time as recorded in the rocks or soil.

    For example, the presence of recycled bricks at an archaeological site indicates the sequence in which the structures were built. Similarly, in geology, if distinctive granitic pebbles can be found in the sediment beside a similar granitic body, it can be inferred that the granite, after cooling, had been uplifted and eroded and therefore was not injected into the adjacent rock sequence.

    Although with clever detective work many complex time sequences or relative ages can be deduced, the ability to show that objects at two separated sites were formed at the same time requires additional information. A coin, vessel, or other common artifact could link two archaeological sites, but the possibility of recycling would have to be considered. It should be emphasized that linking sites together is essential if the nature of an ancient society is to be understood, as the information at a single location may be relatively insignificant by itself.

    Similarly, in geologic studies, vast quantities of information from widely spaced outcrops have to be integrated. Some method of correlating rock units must be found. In the ideal case, the geologist will discover a single rock unit with a unique collection of easily observed attributes called a marker horizon that can be found at widely spaced localities.

    Any feature, including colour variations, textures, fossil content, mineralogyor any unusual combinations of these can be used. It is only by correlations that the conditions on different parts of Earth at any particular stage in its history can be deduced. In addition, because sediment deposition is not continuous and much rock material has been removed by erosionthe fossil record from many localities has to be integrated before a complete picture of the evolution of life on Earth can be assembled.

    Using this established record, geologists have been able to piece together events over the past million years, or about one-eighth of Earth history, during which time useful fossils have been abundant.

    The need to correlate over the rest of geologic time, to correlate nonfossiliferous units, and to calibrate the fossil time scale has led to the development of a specialized field that makes use of natural radioactive isotopes in order to calculate absolute ages.

    The precise measure of geologic time has proven to be the essential tool for correlating the global tectonic processes that have taken place in the past. Precise isotopic ages are called absolute ages, since they date the timing of events not relative to each other but as the time elapsed between a rock-forming event and the present.

    The same margin of error applies for younger fossiliferous rocks, making absolute dating comparable in precision to that attained using fossils. To achieve this precision, geochronologists have had to develop the ability to isolate certain high-quality minerals that can be shown to have remained closed to migration of the radioactive parent atoms they contain and the daughter atoms formed by radioactive decay over billions of years of geologic time.

    In addition, they have had to develop special techniques with which to dissolve these highly refractory minerals without contaminating the small amount about one-billionth of a gram of contained lead and uranium on which the age must be calculated. Since parent uranium atoms change into daughter atoms with time at a known rate, their relative abundance leads directly to the absolute age of the host mineral.

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    In fact, even in younger rocks, absolute dating is the only way that the fossil record can be calibrated.

    Without absolute ages, investigators could only determine which fossil organisms lived at the same time and the relative order of their appearance in the correlated sedimentary rock record. Unlike ages derived from fossils, which occur only in sedimentary rocks, absolute ages are obtained from minerals that grow as liquid rock bodies cool at or below the surface.

    When rocks are subjected to high temperatures and pressures in mountain roots formed where continents collide, certain datable minerals grow and even regrow to record the timing of such geologic events. When these regions are later exposed in uptilted portions of ancient continents, a history of terrestrial rock-forming events can be deduced.

    Episodes of global volcanic activityrifting of continents, folding, and metamorphism are defined by absolute ages. The results suggest that the present-day global tectonic scheme was operative in the distant past as well. Continents move, carried on huge slabs, or plates, of dense rock about km 62 miles thick over a low-friction, partially melted zone the asthenosphere below. In the oceansnew seafloor, created at the globe-circling oceanic ridgesmoves away, cools, and sinks back into the mantle in what are known as subduction zones i.

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    Where this occurs at the edge of a continent, as along the west coast of North and South America, large mountain chains develop with abundant volcanoes and their subvolcanic equivalents. These units, called igneous rockor magma in their molten form, constitute major crustal additions.

    By contrast, crustal destruction occurs at the margins of two colliding continents, as, for example, where the subcontinent of India is moving north over Asia. Great uplift, accompanied by rapid erosion, is taking place and large sediment fans are being deposited in the Indian Ocean to the south. Rocks of this kind in the ancient record may very well have resulted from rapid uplift and continent collision.

    When continental plates collide, the edge of one plate is thrust onto that of the other. The rocks in the lower slab undergo changes in their mineral content in response to heat and pressure and will probably become exposed at the surface again some time later.

    Rocks converted to new mineral assemblages because of changing temperatures and pressures are called metamorphic. Virtually any rock now seen forming at the surface can be found in exposed deep crustal sections in a form that reveals through its mineral content the temperature and pressure of burial.

    Such regions of the crust may even undergo melting and subsequent extrusion of melt magma, which may appear at the surface as volcanic rocks or may solidify as it rises to form granites at high crustal levels. Magmas produced in this way are regarded as recycled crust, whereas others extracted by partial melting of the mantle below are considered primary.

    Even the oceans and atmosphere are involved in this great cycle because minerals formed at high temperatures are unstable at surface conditions and eventually break down or weather, in many cases taking up water and carbon dioxide to make new minerals. If such minerals were deposited on a downgoing i. These components would then rise and be fixed in the upper crust or perhaps reemerge at the surface.

    Such hot circulating fluids can dissolve metals and eventually deposit them as economic mineral deposits on their way to the surface. Geochronological studies have provided documentary evidence that these rock-forming and rock-re-forming processes were active in the past. Seafloor spreading has been traced, by dating minerals found in a unique grouping of rock units thought to have been formed at the oceanic ridges, to million years ago, with rare occurrences as early as 2 billion years ago.

    Other ancient volcanic units document various cycles of mountain building. The source of ancient sediment packages like those presently forming off India can be identified by dating single detrital grains of zircon found in sandstone.

    Magmas produced by the melting of older crust can be identified because their zircons commonly contain inherited older cores. Episodes of continental collision can be dated by isolating new zircons formed as the buried rocks underwent local melting.

    Periods of deformation associated with major collisions cannot be directly dated if no new minerals have formed. The time of deformation can be bracketed, however, if datable units, which both predate and postdate it, can be identified. The timing of cycles involving the expulsion of fluids from deep within the crust can be ascertained by dating new minerals formed at high pressures in exposed deep crustal sections.

    In some cases, it is possible to prove that gold deposits may have come from specific fluids if the deposition time of the deposits can be determined and the time of fluid expulsion is known.

    Where the crust is under tension, as in Iceland, great fissures develop. These fissures serve as conduits that allow black lavacalled basaltto reach the surface. The portion that remains in a fissure below the surface usually forms a vertical black tubular body known as a dike or dyke. Precise dating of such dikes can reveal times of crustal rifting in the past. Dikes and lava, now exposed on either side of Baffin Bayhave been dated to determine the time when Greenland separated from North America—namely, about 60 million years ago.

    Combining knowledge of Earth processes observed today with absolute ages of ancient geologic analogues seems to indicate that the oceans and atmosphere were present by at least 4 billion years ago and that they were probably released by early heating of the planet.

    The continents were produced over time; the oldest preserved portions were formed approximately 4 billion years ago, but this process had begun about by 4.

    Absolute dating allows rock units formed at the same time to be identified and reassembled into ancient mountain belts, which in many cases have been disassociated by subsequent tectonic processes. The most obvious of these is the Appalachian chain that occupies the east coast of North America and extends to parts of Newfoundland as well as parts of Ireland, England, and Norway.

    Relic oceanic crustformed between million and million years ago, was identified on both sides of the Atlantic in this chain, as were numerous correlative volcanic and sedimentary units.

    Evidence based on geologic description, fossil content, and absolute and relative ages leave no doubt that these rocks were all part of a single mountain belt before the Atlantic Ocean opened in stages from about million years ago. Determination of sequence Relative geologic ages can be deduced in rock sequences consisting of sedimentary, metamorphic, or igneous rock units. In fact, they constitute an essential part in any precise isotopic, or absolute, dating program.

    Such is the case because most rocks simply cannot be isotopically dated. Therefore, a geologist must first determine relative ages and then locate the most favourable units for absolute dating. It is also important to note that relative ages are inherently more precise, since two or more units deposited minutes or years apart would have identical absolute ages but precisely defined relative ages. While absolute ages require expensive, complex analytical equipment, relative ages can be deduced from simple visual observations.

    Steno's four laws of stratigraphy. Most methods for determining relative geologic ages are well illustrated in sedimentary rocks. These rocks cover roughly 75 percent of the surface area of the continents, and unconsolidated sediments blanket most of the ocean floor.

    They provide evidence of former surface conditions and the life-forms that existed under those conditions. The sequence of a layered sedimentary series is easily defined because deposition always proceeds from the bottom to the top.

    This principle would seem self-evident, but its first enunciation more than years ago by Nicolaus Steno represented an enormous advance in understanding. Known as the principle of superpositionit holds that in a series of sedimentary layers or superposed lava flows the oldest layer is at the bottom, and layers from there upward become progressively younger. On occasion, however, deformation may have caused the rocks of the crust to tilt, perhaps to the point of overturning them.

    Moreover, if erosion has blurred the record by removing substantial portions of the deformed sedimentary rock, it may not be at all clear which edge of a given layer is the original top and which is the original bottom. Identifying top and bottom is clearly important in sequence determination, so important in fact that a considerable literature has been devoted to this question alone.

    Many of the criteria of top—bottom determination are based on asymmetry in depositional features. Oscillation ripple marks, for example, are produced in sediments by water sloshing back and forth. When such marks are preserved in sedimentary rocks, they define the original top and bottom by their asymmetric pattern. Certain fossils also accumulate in a distinctive pattern or position that serves to define the top side. In wind-blown or water-lain sandstonea form of erosion during deposition of shifting sand removes the tops of mounds to produce what are called cross-beds.

    The truncated layers provide an easily determined depositional top direction. The direction of the opening of mud cracks or rain prints can indicate the uppermost surface of mudstones formed in tidal areas. When a section of rock is uplifted and eroded, as during mountain-building episodes, great volumes of rock are removed, exposing a variety of differently folded and deformed rock units. The new erosion surface must postdate all units, dikes, veins, and deformation features that it crosses.

    Even the shapes formed on the erosional or depositional surfaces of the ancient seafloor can be used to tell which way was up. A fragment broken from one bed can only be located in a younger unit, and a pebble or animal track can only deform a preexisting unit—i. In fact, the number of ways in which one can determine the tops of well-preserved sediments is limited only by the imagination, and visual criteria can be deduced by amateurs and professionals alike.

    One factor that can upset the law of superposition in major sediment packages in mountain belts is the presence of thrust faults. Such faultswhich are common in compression zones along continental edges, may follow bedding planes and then cross the strata at a steep angle, placing older units on top of younger ones.

    In certain places, the fault planes are only a few centimetres thick and are almost impossible to detect. Relative ages also can be deduced in metamorphic rocks as new minerals form at the expense of older ones in response to changing temperatures and pressures. In deep mountain roots, rocks can even flow like toothpaste in their red-hot state.
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