The Late. Payment Surcharge shall be governed as per the provisions of Electricity (Late Payment Surcharge) Rules, 2021 issued by Ministry of Power, Government of India vide notification dated 22.02.2021 and subsequent amendments or replacements thereof issued from time to time.
The Late. Usage Discount shall also not apply unless the Receiving Party notifies the Providing Party that it has not received the usage records within five (5) business days of the time the Receiving Party discovers, or should have discovered using reasonable business practices, that it has not received the usage records.
The Late. Usage Discount shall only apply where the late usage hinders the Receiving Party's ability to promptly xxxx its customers.
The Late. Registration Payments will be equal to 1% of the purchase price paid for the Common Shares purchased by such Investor and not previously sold by such Investor for each 30 business days after the Required Effective Date (but in no event to exceed 12% in the aggregate). The Late Registration Payments will be prorated on a daily basis during the 30 business day period and will be paid to the Initial Investors by check within five business days after the earlier of (i) the end of the 30 business days following the Required Effective Date or (ii) the effective date of the Registration Statement.
The Late. Wisconsinan Laurentide Ice Sheet reached its terminal position south of Block Island at the last glacial maximum, coinciding with the low-stand in eustatic sea level around 26,000 yBP, before beginning to retreat northward (Boothroyd and Xxxxxx, 2002; Xxxx et al., 2002; Xxxxxxx and Fairbanks, 2006; Xxxxx and Borns jr., 1986). As the glacier retreated, melt-water issuing from the ice deposited sediment in a variety of depositional environments (Xxxxxxxxx and Xxxxxxxxx, 1987; Stone and Stone, 2005) on what is now the southern Rhode Island shoreface and outer continental shelf. Of particular interest to this study are previously identified large glacial deltas, which underlie the modern coastal lagoons and extend south into Block Island Sound (Figure 3). These deltas were deposited into Glacial Lake Block Island sometime before 21,000 yBP (Oakley and Boothroyd, 2013; Oakley, 2012), prior to sea level inundating the study area. Sub-bottom seismic reflection profiles collected by Xxxxxx (2012) from the present upper shoreface and inner continental shelf showed southerly dipping (5 - 15º) reflectors offshore of the Rhode Island south shore, interpreted to have been deposited in a delta slope depositional environment (Figure 4) (Oakley, 2012), These were hypothesized to contain significant volumes of sand and gravel. Characterizing the location, sedimentology, and volume of these deltas was a primary focus of this study.
