B. T. Lowne suggests that despite the complexity of the subject, the darkness of misconceptions should not return, given the efforts of scientists like Fritz Müller, Weismann, and Lubbock. Mr. Laughton's concept of 'aspect' is fundamental to the theory of surfaces, as every surface has an aspect, defined as the direction of a normal at any point. This concept is essential for understanding planes, their angles, tangents, and intersections. The term 'aspect' is not new, as noted by Mr. Proctor and Sir W. R. Hamilton. It is a precise and technical term that is needed in the reconstruction of geometry. Position is a key attribute of planes, and while parallel planes share the same aspect, their positions differ. In a separate note, the author discusses the cause of low barometric pressure, noting that the law of deflection of winds is now widely accepted. The author confirms that the lowest pressures are not at the poles but near Iceland and the Aleutian Islands. The low temperature at the poles explains the course of Atlantic storms. The author also discusses the notation for acceleration, noting that while 'j' is used in some works, the notation of Newton's fluxions is more appropriate and widely applicable. The author suggests that the notation of Newton's fluxions is more suitable for all stages of a student's learning.B. T. Lowne suggests that despite the complexity of the subject, the darkness of misconceptions should not return, given the efforts of scientists like Fritz Müller, Weismann, and Lubbock. Mr. Laughton's concept of 'aspect' is fundamental to the theory of surfaces, as every surface has an aspect, defined as the direction of a normal at any point. This concept is essential for understanding planes, their angles, tangents, and intersections. The term 'aspect' is not new, as noted by Mr. Proctor and Sir W. R. Hamilton. It is a precise and technical term that is needed in the reconstruction of geometry. Position is a key attribute of planes, and while parallel planes share the same aspect, their positions differ. In a separate note, the author discusses the cause of low barometric pressure, noting that the law of deflection of winds is now widely accepted. The author confirms that the lowest pressures are not at the poles but near Iceland and the Aleutian Islands. The low temperature at the poles explains the course of Atlantic storms. The author also discusses the notation for acceleration, noting that while 'j' is used in some works, the notation of Newton's fluxions is more appropriate and widely applicable. The author suggests that the notation of Newton's fluxions is more suitable for all stages of a student's learning.