Time the calendar
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The document discusses time and calendars. It explains how to tell time using both analog and digital clocks, how to add and subtract times, and how to convert between 12-hour and 24-hour time. It also discusses leap years on the calendar and the main time units like seconds, minutes, hours, days, weeks, months, years, decades, centuries and millennia. There are examples and practice problems provided about calculating times, converting between time formats, and identifying leap years.
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1. The document discusses time systems including 12-hour and 24-hour formats. It provides examples of converting times between the two formats, such as 1:00 PM = 13:00.
2. Instructions are given for using a.m. and p.m. indicators as well as four-digit times in the 24-hour format. Examples are shown of writing times of day like 6:35 AM as 06:35.
3. Several practice exercises are included to have the reader practice converting times between 12-hour and 24-hour formats themselves. Times are given to convert in both directions to reinforce the concepts.
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The document provides instructions for telling time in English using analog clocks. It explains that in English, the minutes are said before the hour rather than after as in Greek. For example, 9:15 would be "a quarter past nine" instead of "nine and a quarter." It also describes the hands on an analog clock, with the long minute hand making a full rotation in 60 minutes and the short hour hand indicating the hour. Examples are given for telling times like "half past," "quarter past/to," and using a.m. or p.m. to indicate times before or after noon.
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The document discusses calculating time periods between start and end times. It provides examples of calculating time periods in hours and minutes for events occurring on different days from morning to evening. The time periods are calculated by subtracting the start time from the end time, and periods crossing midnight are split into before and after midnight segments.
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Lat and long time zones 2
Latitude and longitude are used to locate places on maps. Lines of latitude run horizontally around the Earth and are measured in degrees from the equator (0 degrees) to the poles (90 degrees North and South). Lines of longitude run vertically and are also called meridians, measured in degrees East and West from the prime meridian in Greenwich, England (0 degrees). The intersection of lines of latitude and longitude create a grid that can be used to specify any location on Earth. Time zones, which shift in 15 degree widths, use latitude and longitude to demarcate one hour of time difference between each zone.
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Masa & waktu 1
1. The document discusses time systems including 12-hour and 24-hour formats. It provides examples of converting times between the two formats, such as 1:00 PM = 13:00.
2. Instructions are given for using a.m. and p.m. indicators as well as four-digit times in the 24-hour format. Examples are shown of writing times of day like 6:35 AM as 06:35.
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The document provides instructions for telling time in English using analog clocks. It explains that in English, the minutes are said before the hour rather than after as in Greek. For example, 9:15 would be "a quarter past nine" instead of "nine and a quarter." It also describes the hands on an analog clock, with the long minute hand making a full rotation in 60 minutes and the short hour hand indicating the hour. Examples are given for telling times like "half past," "quarter past/to," and using a.m. or p.m. to indicate times before or after noon.
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The document discusses calculating time periods between start and end times. It provides examples of calculating time periods in hours and minutes for events occurring on different days from morning to evening. The time periods are calculated by subtracting the start time from the end time, and periods crossing midnight are split into before and after midnight segments.
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The document discusses Earth's relationship to the sun and solar radiation. It provides an overview of the solar system, including its formation and structure. It describes Earth's place in the system and orientation relative to the sun. It then discusses solar radiation, including electromagnetic radiation, the composition and spectrum of sunlight, and how the intensity and distribution of solar energy varies over Earth and between seasons due to its orientation within the solar system.
Lat and long time zones 2
Latitude and longitude are used to locate places on maps. Lines of latitude run horizontally around the Earth and are measured in degrees from the equator (0 degrees) to the poles (90 degrees North and South). Lines of longitude run vertically and are also called meridians, measured in degrees East and West from the prime meridian in Greenwich, England (0 degrees). The intersection of lines of latitude and longitude create a grid that can be used to specify any location on Earth. Time zones, which shift in 15 degree widths, use latitude and longitude to demarcate one hour of time difference between each zone.
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The document provides information about converting between 12-hour and 24-hour time formats. It explains that the 12-hour clock uses a.m. and p.m. while the 24-hour clock uses hours (H) and does not require a.m. or p.m. Converting between the two involves adding or subtracting 12 based on whether the time is before or after noon. The document also includes examples of converting times between the 12-hour and 24-hour formats.
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- The ozone layer is found 20-30km above the Earth's surface and absorbs UV radiation.
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- Significant ozone depletion up to 50% has been observed over the Antarctic region, known as the ozone hole.
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1) Fossils, their types and classification of organisms. 2) Principles of relative dating such as superposition and cross-cutting relations. 3) Dendrochronology and its use in dating features. 4) An overview of the geologic time scale from the Hadean Eon to periods in the Paleozoic, Mesozoic, and Cenozoic eras.
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This PowerPoint outlines how to calculate different times throughout the world for students living in Queensland, Australia.
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The document discusses time zones around the world, noting that Greenwich, England is located at 0 degrees longitude and is used to measure time from, with time zones adding or subtracting one hour for every 15 degrees east or west; it explains that international date line follows the 180th meridian and results in a one day difference when crossing it west to east; and time zone boundaries sometimes adjust slightly within countries to avoid confusion by keeping entire states or provinces within the same time zone.
Earth Systems and Resources
An overview of the Earth's systems and resources from earth science to atmosphere to water use to soil.
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The document discusses the structure of the Earth by comparing it to an apple. It explains that both have a thin outer crust/skin, a thick inner core, and layers in between. The Earth has an inner solid core and outer liquid core of iron and nickel. Between the core and crust is the mantle, made of solid but hot rock. The crust floats on the mantle and is divided into thinner oceanic crust and thicker continental crust made of different materials.
STRUCTURE OF THE ATMOSPHERE
The document discusses the structure and composition of Earth's atmosphere. It is divided into four layers: the troposphere, stratosphere, mesosphere, and thermosphere. Each layer has distinct temperature and chemical characteristics. The troposphere contains around 80% of the atmosphere and is where weather occurs. Temperatures decrease with height in the troposphere. The stratosphere has temperatures that increase with height due to ozone absorbing UV radiation. The mesosphere has temperatures that decrease rapidly with no gases to absorb radiation.
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The document provides information about converting between 12-hour and 24-hour time formats. It explains that the 12-hour clock uses a.m. and p.m. while the 24-hour clock uses hours (H) and does not require a.m. or p.m. Converting between the two involves adding or subtracting 12 based on whether the time is before or after noon. The document also includes examples of converting times between the 12-hour and 24-hour formats.
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This document provides examples of solving time-related problems by converting between hours and minutes. It gives step-by-step workings for converting times such as 6.15 hours to hours and minutes, finding the number of minutes in periods like 3 hours and 1/4 hours, and converting total minutes to hours and minutes. Examples are also given for calculating elapsed time between times on different days and the total time taken by adding periods spent on different days.
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The document provides instruction on telling time using a 12-hour clock. It explains that the hour hand indicates the hour since 12:00 and the minute hand tracks minutes within the current hour. Several examples are given of writing times such as 7:10 or 11:25 in numeric format. The document concludes with examples that ask the reader to determine the hour and minutes shown on sample clocks.
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This document provides information about telling time on both analog and digital clocks. It includes illustrations of clock faces showing the positions of the hour and minute hands for different times. The text then gives examples of stating the time in terms like "five past eight" or "ten to seven". Finally, there is a short dialogue demonstrating asking and stating the time.
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Time the calendar
- 2. TIME
- 3. ANALOGUE Hands of the analogue clock
- 4. DIGITAL
- 5. FIVE O’CLOCK
- 6. “HALF PAST FIVE “ OR “FIVE – THIRTY”
- 7. SIX O’CLOCK
- 8. PROBLEMS Display these times using analogue and digital: Half past ten Quarter past one Ten to eleven Three O’clock
- 9. ADDING AND SUBTRACTING TIME What is 2:45 + 1:10 ? What is 2:45 + 1:20 ? What is 4:10 - 1:05 ? What is 4:10 - 1:35 ?
- 10. PROBLEMS What is the time: a) 20 minutes after 10.40 ? b) 30 minutes before 8.40 ? c) 10 minutes before 6.05 ? d) 1.30 hours after 11.45 ?
- 11. 24 - HOUR CLOCK Morning times 0001 – 11 59 am (Ante Meridian)) Afternoon / evening times
- 12. CONVERTING FROM 24 HOUR CLOCK TO AM / PM Converting from 24 hour clock to AM / PM 0000 to 0059 0100 to 1159 1200 to 1259 1300 to 2359 add 12 hours straight conversion to AM straight conversion to PM subtract 12 hours EXAMPLES: 0000 --> 12 midnight 0015 --> 12:15 AM 0030 --> 12:30 AM 0059 --> 12:59 AM EXAMPLES: 0100 --> 01:00 AM 0300 --> 03:00 AM 0700 --> 07:00 AM 0830 --> 08:30 AM 1000 --> 10:00 EXAMPLES: 1200 --> 12 noon 1215 --> 12:15 PM 1230 --> 12:30 PM 1259 --> 12:59 PM EXAMPLES: 1300 --> 01:00 PM 1500 --> 03:00 PM 1800 --> 06:00 PM 2030 --> 08:30 PM 2215 --> 10:15
- 13. PROBLEMS Change these 24-hour clock times to am/pm time: 0945 1500 0430 1650 2020 0815 2330 1215 0020
- 14. PROBLEMS Write these times using the 24-hour clock: 1. Half past seven in the morning 2. Twenty to nine at night 3. Five to four in the afternoon 4. Quarter to four in the morning 5. Ten past eight at night 6. Twenty five past two in the
- 15. THE CALENDAR
- 16. LEAP YEARS
- 17. PROBLEMS Which of these are leap years? 2004 1967 1942 1900 2100 2000
- 18. MAIN TIME UNITS 1 second 1 week = 7 days 1 decade = 10years 1 minute = 60 seconds 1 month 1 century = 100 years 1 hour = 60 minutes 1 year 1 millennium = 1000 years 1 day = 24 hours
- 19. PROBLEMS How many minutes are there in 3 hours? How many hours are there in 2 days? How many minutes are there in half an hour? How many months are there in 4 years? How many decades are there in a