Enter an angle (degrees or radians) into the calculator to find the equivalent time for a rotating clock hand. By default, the “Angle ↔ Time (Minute hand)” tab assumes 360° corresponds to 60 minutes (one full rotation of the minute hand).

Angle To Time Calculator

Angle ↔ Time (Minute hand)
Hour hand
Second hand
Custom period
Clock hands angle

Enter any 1 value to calculate the missing variable

Assumes a 60-minute full rotation (minute hand).

Related Calculators

Angle To Time Formula

T = A / 6

Variables:

  • T is the time (minutes) for the minute hand to sweep angle A (i.e., 360° = 60 minutes).
  • A is the angle (degrees).

For the minute hand, convert angle to time by multiplying by 1/6 ≈ 0.1666667 (since 60/360 = 1/6). The general form for any rotating system is T = (A / 360) × P, where P is the full rotation period. Each clock hand has a different angular rate: the minute hand moves 6°/min, the hour hand moves 0.5°/min, and the second hand moves 6°/s (360°/min).

Angle (Degrees) to Time Conversion Table (minute hand: Time = Angle × 1/6 min/deg)
Degrees (°) Minutes (min) Seconds (s) Hours (h)
0.50.08350.001
10.167100.003
20.333200.006
30.500300.008
50.833500.014
7.51.250750.021
101.6671000.028
122.0001200.033
152.5001500.042
203.3332000.056
22.53.7502250.063
305.0003000.083
366.0003600.100
457.5004500.125
6010.0006000.167
9015.0009000.250
12020.00012000.333
18030.00018000.500
27045.00027000.750
36060.00036001.000
Uses Time (minutes) = Angle (degrees) × (60/360) = Angle/6. Equivalences (minute hand): 1° = 1/6 min = 10 s; 360° = 60 min = 1 h. If angle is in radians, convert first: 1 rad ≈ 57.2958°.

Angular Rates of Real-World Rotating Systems

Angle-to-time conversion applies to any system with a known rotation period. The table below compares the angular rate of common rotating systems, which determines how much angle accumulates per unit of time. Every row uses the same underlying formula: angular rate = 360° / period.

Angular Rate Comparison: Real-World Rotating Systems
System Full Rotation Period Rate (°/min) Rate (°/s) Notes
Clock second hand60 s3606Fastest standard clock hand
Clock minute hand60 min60.1Base case for this calculator
Clock hour hand12 h (720 min)0.50.00833Moves 30° per hour mark
Earth (solar day)24 h0.250.004167Basis for time zones (15°/hr)
Earth (sidereal day)23 h 56 m 4 s0.250680.004178True rotation vs. fixed stars
Earth around Sun365.25 days0.0006850.0000114~0.9856°/day of orbital motion
Moon around Earth27.32 days0.009160.000153Sidereal orbital period
Typical vinyl record (33⅓ RPM)1.8 s12,000200Standard LP speed
Helicopter main rotor (~300 RPM)0.2 s108,0001,800Typical cruise RPM
Car engine (idle ~800 RPM)0.075 s288,0004,800Varies by engine
Hard drive platter (7,200 RPM)0.00833 s2,592,00043,200Standard desktop HDD
Angular rate = 360° / period. The solar vs. sidereal day difference (3 min 56 s) exists because Earth must rotate slightly more than 360° each solar day to compensate for its orbital motion around the Sun.

Hour Angle in Astronomy and Celestial Navigation

Astronomers formalized the angle-to-time relationship long before mechanical clocks existed. In celestial coordinate systems, a star's position is measured using right ascension, which is expressed in hours, minutes, and seconds rather than degrees. The conversion is exact: 24 hours = 360°, making 1 hour of right ascension equal to exactly 15°, 1 minute of right ascension equal to 0.25°, and 1 second equal to 0.004167°.

The hour angle of a celestial object is the angle between the observer's meridian and the object's position, measured westward in time units. When an object has an hour angle of 0h, it is on the meridian and at its highest point in the sky (transit). An hour angle of 6h means the object is 90° west of the meridian and set 6 hours ago if on the celestial equator. This framework allowed sailors to determine longitude with a sextant and an accurate chronometer before GPS: measuring the Sun's hour angle at local noon and comparing it to Greenwich Mean Time gave longitude directly in degrees (15° per hour of difference).

The Earth's actual sidereal rotation rate is 360° per 23 hours 56 minutes 4.09 seconds, not 24 hours. The extra 3 minutes 55.91 seconds per day accumulates because Earth is simultaneously orbiting the Sun, requiring a small additional rotation to bring the Sun back to the same apparent position. This adds approximately 0.9856°/day of "extra" rotation, making the solar-day angular rate slightly faster than the sidereal rate.

Time Zones and the 15-Degree Rule

The modern time zone system is a direct product of angle-to-time conversion. Because Earth completes 360° in 24 hours, each hour of time corresponds to exactly 15° of longitude. The 24 standard time zones are each 15° wide, which is why crossing a standard time zone boundary shifts the clock by exactly one hour. In practice, time zone boundaries follow political and geographic borders rather than strict meridians, so actual zones deviate from the ideal 15° bands.

Sundials used this relationship for thousands of years before clocks were invented. Each hour line on a sundial is spaced 15° apart (for a vertical dial at the equator), since the Sun appears to move 15°/hour across the sky. The equation of time, which describes the difference between apparent solar time (what a sundial reads) and mean solar time (what a clock reads), varies by up to 16 minutes 33 seconds across the year due to Earth's elliptical orbit and axial tilt. This means a sundial is only perfectly accurate on approximately four dates per year (around April 15, June 13, September 1, and December 25).

FAQs

What is the significance of converting angles to time?

Any rotating system with a fixed period links angle directly to elapsed time through the ratio T = (A / 360) × P. The relationship appears in clock mechanics, astronomy, celestial navigation, motor engineering, and signal processing. On this page, the basic formula assumes a clock-style mapping for the minute hand: 360° = 60 minutes.

Why does 1° of longitude equal 4 minutes of time?

Earth rotates 360° in 24 hours, giving 15° per hour. Dividing further: 15° per 60 minutes = 0.25° per minute, or equivalently 1° per 4 minutes. This is the conversion sailors used for centuries to find their longitude at sea by comparing local solar noon to a reference clock set to Greenwich time.

What is the difference between a solar day and a sidereal day in angle terms?

A sidereal day is 23 hours 56 minutes 4.09 seconds, during which Earth rotates exactly 360° relative to distant stars. A solar day is 24 hours, during which Earth rotates approximately 360.9856° relative to the Sun. The extra 0.9856° per day is required to compensate for Earth's orbital motion. Over a full year, these extra daily increments sum to one full extra rotation (360°), which is why there are 366 sidereal days in a year but only 365 solar days.

Can this formula be used for any rotating system?

Yes. For any system with a known period P, use T = (A / 360) × P, with A in degrees and T and P in the same time units. The Custom Period tab accepts any rotation period in seconds, minutes, or hours, making it applicable to motors, planetary bodies, spinning machinery, or any other periodic rotator.

How accurate is the angle-to-time conversion?

The conversion is exact within the model (the only error comes from input rounding). The precision limit is the accuracy of the rotation period itself. For a mechanical clock, the period drifts slightly with temperature and spring tension. For Earth's rotation, the period itself changes measurably over geological time due to tidal braking from the Moon, lengthening the day by roughly 1.4 milliseconds per century.

Is there a way to convert time back to angle?

Yes. For the minute hand: A = 6T (degrees, T in minutes). For the hour hand: A = 0.5T (degrees, T in minutes). For the second hand: A = 6T (degrees, T in seconds). For any period P: A = (T / P) × 360, with T and P in matching units. The calculator above solves in both directions for all three clock hands and custom periods.