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The Current Local Date and Time in Chapada, Brazil (BR)

Name: Chapada
Address: Chapada, BR

Time Zone America/Sao_Paulo

21:32:20

Local Time Date and Timezone

Where is Chapada? (Brazil, BR)

Chapada is a city located in Brazil (BR).
Latitude -28.05528 Longitude -53.06778

Chapada location on the Brazil (BR) map

Information about Chapada

City: Chapada
Country: Brazil (BR)
Latitude: -28.05528
Longitude: -53.06778
Time Zone: America/Sao_Paulo

Time zone and UTC offset ofChapada

Chapada, Brazil is in the America/Sao_Paulo time zone, which is currently UTC-3. Daylight saving time is not observed in this time zone, so the offset stays the same all year.

Current time difference with other cities

Chapada is 4 hours behind London
Chapada is 1 hour ahead of New York
Chapada is 4 hours ahead of Los Angeles
Chapada is 7 hours behind Dubai
Chapada is 12 hours behind Tokyo
Chapada is 14 hours behind Sydney

Frequently asked questions about time inChapada

What time zone is Chapada in?

Chapada, Brazil is in the America/Sao_Paulo time zone (currently UTC-3).

Does Chapada observe daylight saving time?

No, the clocks do not change during the year in this time zone.

What is the time difference between Chapada and New York?

Chapada is 1 hour ahead of New York (the difference can change when either place switches to or from daylight saving time).

What are the coordinates of Chapada?

Chapada is located at latitude -28.05528 and longitude -53.06778.

Sunrise, sunset and moon phase inChapada today

Astronomical data for October 15, 2026 in Chapada, calculated for the America/Sao_Paulo time zone. All times are local.

Sun

Sunrise: 05:56
Solar noon: 12:18
Sunset: 18:41
Length of day: 12 h 45 min

Moon

Moon phase: Waxing Crescent
Illumination: 26%
Moon age: about 5.0 days
Moonrise: 08:56
Moonset: 23:36

Other cities inBrazil

All cities and towns in Brazil

City of Chapada

A chapada (Portuguese pronunciation: [ʃaˈpadɐ]) is a plateau found in the Brazilian Highlands. The chapadas, which are usually described as mountain ranges, are capped by horizontal strata of sandstone. They show the original surface, which has been worn away by the rivers, leaving here and there broad flat-topped ridges between river basins and narrower ranges of hills between river courses. From the valleys their rugged, deeply indented escarpments, stretching away to the horizon, they have the appearance of a continuous chain of mountains.
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