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Deposits.com is a one-stop-shop for the best Financial Advisors, Financial Literacy Content, Tax & Mortgage Calculators, and more. Better for business Own a business? Deposit definition is - to place especially for safekeeping or as a pledge; especially, economics: to put in a bank. How to use deposit in a sentence. Deposits are also required on many large purchases, such as real estate or vehicles, for which sellers require payment plans. Financing companies typically set these deposits at a certain.

Deposit definition: A deposit is a sum of money which is part of the full price of something, and which you. Meaning, pronunciation, translations and examples.

Chase QuickDeposit℠

Deposit checks with the Chase Mobile^® app.

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Use Chase QuickDeposit℠ on the Chase Mobile^® app to deposit your checks and access your funds quickly.

Save a trip to the branch and deposit checks on your schedule, virtually anytime and anywhere.

Deposit checks securely from your mobile phone or tablet. We protect your information and never store your passwords or check deposit data and images on your mobile device.

How to get started

Watch how it works with this helpful how-to video.

Depositesfiles

Choose 'Deposit checks' in the navigation menu of your Chase Mobile^® app and choose the account. 

Enter the check amount and tap 'Front'. With our new 'Auto Capture' feature, the picture of the front and back of the endorsed check will be captured — or you can choose to take the pictures manually.

Confirm the details, submit and you're done.

Common questions answered

How does Chase QuickDeposit℠ work?

In the Chase Mobile^® app, choose “Deposit Checks” in the navigation menu and select the account. Enter the amount of the check and tap 'Front'. With our 'Auto Capture' feature, the picture of the front and back of the endorsed check will be captured — or you can choose to take the pictures manually. Verify your information and submit your deposit. After you submit, you can deposit another check or view the receipt. You’ll get an email when your deposit is received — and another when it’s accepted. If the deposit is rejected, you’ll also get an emailed explanation. Remember to properly endorse the back of the check with your signature and 'For electronic deposit only at Chase.'

When will my funds be available?

Deposits submitted before 11 PM Eastern time on a business day generally will be available by the next business day. Deposits submitted after 11 PM or on a non-business day will be processed the next business day. However, we may delay availability if we require further review of the deposit. Any information about delayed availability will be provided in the Secure Message Center, which is accessible in the main navigation menu.

What should I do with my check(s) after I’ve deposited it?

After you complete your transaction, write “deposited” and the date of deposit on the face of the check. Please retain the marked check for two business days or until you receive our notification that your QuickDeposit has been accepted. After that time, you may destroy it.

Have more questions?

24/7 access to deposit funds

• Chase QuickDeposit℠ — Securely deposit checks from almost anywhere.
• Chase ATMs — Conveniently deposit up to 30 checks and cash at most ATMs.
  
• Direct deposit — Automatically deposit paychecks.

Deposits

Pay bills quickly & conveniently

• Online Bill Pay — Pay rent, mortgage, utilities, credit cards, auto and other bills.
• Chase QuickPay^® with Zelle^® — Send and receive money from almost anyone with just a mobile number or email address.

Helpful technology that saves you time and keeps you in the know

Deposits Current Assets

• Paperless statements — Digitally access up to 7 years of statements.
• Account alerts — Monitor finances, avoid overdrafts and more.
• Chase text banking — Check balances and transaction history with a text.

Mineral deposits form because some medium serves as a concentrating and transporting agent for the ore minerals, and some process subsequently causes the transporting agent to precipitate, or deposit, the minerals. Examples of concentrating and transporting agents are groundwater, seawater, and magma; examples of precipitating processes are boiling (as in a hot spring), the cooling of a hot solution, the crystallization of a magma, and a chemical reaction between a solution and the rocks through which it flows. The same kinds of concentrating and transporting agent and the same kinds of precipitating process are involved in the formation of deposits of both geochemically abundant and geochemically scarce metals.

There are six principal concentrating and transporting agents. Together with the classes of deposit that they form, these agents are discussed below.

Magmatic concentration

Magma is molten rock, together with any suspended mineral grains and dissolved gases, that forms when temperatures rise and melting occurs in the mantle or crust. When magma rises to Earth’s surface through fissures and volcanic vents, it is called lava. Lava cools and crystallizes quickly, so that igneous rocks formed from lava tend to consist of tiny mineral grains. (Sometimes cooling can be so rapid that mineral grains cannot form and a glass results.) Underground magma, on the other hand, cools and crystallizes slowly, and the resulting igneous rocks tend to contain mineral grains at least one-half centimetre (about one-quarter inch) in diameter.

Pegmatite deposits

The crystallization of magma is a complex process because magma is a complex substance. Certain magmas, such as those which form granites, contain several percent water dissolved in them. When a granitic magma cools, the first minerals to crystallize tend to be anhydrous (e.g., feldspar), so an increasingly water-rich residue remains. Certain rare chemical elements, such as lithium, beryllium, and niobium, that do not readily enter into atomic substitution in the main granite minerals (feldspar, quartz, and mica) become concentrated in the water-rich residual magma. If the crystallization process occurs at a depth of about five kilometres or greater, the water-rich residual magma may migrate and form small bodies of igneous rock, satellitic to the main granitic mass, that are enriched in rare elements. Such small igneous bodies, called rare-metal pegmatites, are sometimes exceedingly coarse-grained, with individual grains of mica, feldspar, and beryl up to one metre across. Pegmatites have been discovered on all continents, providing an important fraction of the world’s lithium, beryllium, cesium, niobium, and tantalum. Pegmatites also are the major source of sheet mica and important sources of gemstones, particularly tourmalines and the gem forms of beryl (aquamarine and emerald).

Carbonatite deposits

Carbonatites are igneous rocks that consist largely of the carbonate minerals calcite and dolomite; they sometimes also contain the rare-earth ore minerals bastnaesite, parisite, and monazite, the niobium ore mineral pyrochlore, and (in the case of the carbonatite deposit at Palabora in South Africa) copper sulfide ore minerals. The origin of carbonatite magma is obscure. Most carbonatites occur close to intrusions of alkaline igneous rocks (those rich in potassium or sodium relative to their silica contents) or to the ultramafic igneous rocks (rocks with silica contents below approximately 50 percent by weight) known as kimberlites and lamproites. These associations suggest a common derivation, but details of the way that carbonatite magmas might concentrate geochemically scarce metals remain conjectural.

Carbonatites have been found on all continents; they also range widely in age, from deposits in the East African Rift Valley that were formed during the present geologic age to South African deposits dating from the early Proterozoic Eon (2.5 billion to 543 million years ago). Many carbonatites are mined or contain such large reserves that they will be mined someday. Among the most important are Mountain Pass, California, U.S., a major source of rare earths; the Loolekop Complex, Palabora, South Africa, mined for copper and apatite (calcium phosphate, used as a fertilizer), plus by-products of gold, silver, and other metals; Jacupiranga, Brazil, a major resource of rare earths; Oka, Quebec, Canada, a niobium-rich body; and the Kola Peninsula of Russia, mined for apatite, magnetite, and rare earths.