Answer:
True
Explanation:
It is a sprirical and the outermost region of the solar system.
Answer:
A) Energy acquisition and use, using environmental and genetic information for evolution
Explanation:
The process of the movement of the flower towards sunlight , is known as the heliotropism .
It enables in keeping the flower visible and warm for pollinators .
And as the flower is pollinated and forms hard seed .
And for young flowers , the process is to maximize the process of photosynthesis .
It enables to track the sun with 24 biological clock , and after sun set the flower faces towards the east , and wait for the sun to rise .
Answer:
On May 14 Indonesia’s constitutional court ruled to modify the language of a 1999 law, effectively placing millions of hectares of previously government-controlled forest land back into the hands of Indigenous Peoples.
The ruling clarified Indonesia’s classification of forest land, separating state forests from public forests and dividing public forests into either customary or individual forests. Previously, all customary forests had been under state control; now, the rights for customary forests have been handed back to the Indigenous inhabitants.
Explanation:
A gravel covered plain is called a Reg. A reg is a desert basin where the sand has been blown away leaving a gravel covered plain.
Answer: A - P.M. Grootes, K.M. Cuffey, and J.M. Bolzan, among others.
Explanation: Dr. Anandakrishnan collaborated and coauthored with all of the people listed above and has worked with many other people.
During the year 1994, Dr. Sridhar Anandakrishnan collaborated with Kurt M Cuffey, Richard B Alley, Pieter M Grootes and John M Bolzan on the topic 'Calibration of the δ18O isotopic paleothermometer for central Greenland, using borehole temperatures'
They calibrated the δ 18O paleo-thermometer for central Greenland using borehole temperatures, a thermal model forced by a measured δ 18O record and a formal inverse technique. The calibration is determined mostly by temperature fluctuations of the last several centuries, including the Little Ice Age.
Results are generally insensitive to model variables, including initial condition, basal boundary condition, parameterization of snow thermal properties, ice thickness and likely errors in temperature and isotope measurements. Results of this borehole calibration also seem to be in agreement with modern spatial gradients of δ 18O and temperature.
They suggest that calibrations of isotopic paleothermometers using borehole temperatures are a useful paleoclimate tool because they are independent of spatial gradients and include the effects of prehistoric temperatures.
