Investing in Apartment Buildings

The 10-Minute Offer for Apartment Buildings

This ebook teaches you the proven and tested system for making offers on apartment buildings and getting the deal in no time at all! You will control the entire process, and you will learn every detail that you need to clear. You will learn the tips and tricks for working with brokers and how to make sure that the deal falls completely in your favor. Investing in apartment buildings has the potential to be one of the most lucrative businesses that you get in to, because the right building can turning huge amounts of profit without having to spend too much time working for that money. With this ebook, you can get started on the right foot by making sure that you get the deal with plenty of money left to spare. You will cut the deal of a lifetime in 10 minutes or less. It doesn't have to take much time at all to make money! More here...

The 10Minute Offer for Apartment Buildings Summary

Rating:

4.7 stars out of 12 votes

Contents: Ebook
Author: Michael Blank
Price: $99.00

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My The 10Minute Offer for Apartment Buildings Review

Highly Recommended

I've really worked on the chapters in this book and can only say that if you put in the time you will never revert back to your old methods.

In addition to being effective and its great ease of use, this eBook makes worth every penny of its price.

Liquefaction and levees potential double disaster in the american midwest

Sudden shaking of certain types of water-saturated sands and muds turns these once-solid sediments into a slurry having a liquidlike consistency. Liquefaction occurs when shaking causes individual grains in the soil to move apart, then water moves between the grains, making the whole water sediment mixture behave like a fluid. Earthquakes often cause liquefaction of sands and muds, and any structures built on soils or sediments that liquefy may suddenly sink into them as if they were resting on a thick fluid. Liquefaction causes sand to bubble to the surface during earthquakes, forming mounds up to several tens of feet ( 10 m) high, known as sand volcanoes, and ridges of sand to squeeze into cracks in the Earth. Liquefaction is responsible for the sinking of sidewalks, telephone poles, building foundations, and other structures during earthquakes. Famous examples of liquefaction occurred in the 1964 Alaskan earthquake, when entire neighborhoods slid toward the sea on liquefied sand...

Threats and Responses Associated with Rapid Climate Change in Metropolitan New York

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Metropolitan New York is vulnerable to coastal flooding and widespread damage to urban infrastructure, commercial structures and residential neighborhoods from both seasonal hurricanes and extra-tropical storms. A significant portion of the metropolitan area lies less than 3 m above mean sea level in total covering an area of about 260 km2 (see Figure 9.1). Many types of structures are located within this low-lying region, including commercial properties and financial institutions, apartment buildings and private dwellings, hospitals, police and fire stations, marine transportation terminals, three major airports, heliports, numerous underground railroad and subway lines (with associated station entrances and ventilation shafts), highways, bridge access roads, tunnels, power plants, the underground steam district heating system, electrical and communication networks, landfills, 14 waste water treatment facilities and 770 combined sewer overflows with their tide gate regulators...

Liquefaction

Liquefaction occurs where the shaking causes individual grains to move apart, then water moves up in between the individual grains, making the whole water sediment mixture behave like a fluid. Earthquakes often cause liquefaction of sands and muds. Any structures built on sediments that liquefy may suddenly sink into them as if resting on a thick fluid. Liquefaction caused the Bootlegger shale in the 1964 Alaskan earthquake to become suddenly so weak that it destroyed Turnagain Heights. Liquefaction during earthquakes also causes sinking of sidewalks, telephone poles, building foundations, and other structures. One famous example of liquefaction occurred in the Japan earthquake (1964), where entire rows of apartment buildings rolled onto their sides but were not severely damaged internally. Liquefaction also causes sand to bubble to the surface during earthquakes, forming mounds up to several tens of feet high, known as sand volcanoes, or ridges of sand.

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